bayswater uranium corporation - Government of Newfoundland and

Transcription

SECOND YEAR ASSESSMENT REPORT ON THE
BAYSWATER/UCORE JOINT VENTURE MAKKOVIK
RIVER URANIUM PROJECT
CENTRAL MINERAL BELT, LABRADOR
Licenses:
012775M, 012777M, 012780M, 12818M – 012822M, 012825M, 012786M – 012788M,
012791M, 012801M, 012803M, 012798M, 012790M, 012793M – 012796M, 012829M,
012830M - 012832M, 012784M, 012808M, 012747M, 012809M, 012735M, 012768M
NTS Mapsheets:
13J/14, 13J/11, 13J/12
BAYSWATER URANIUM CORPORATION
510 Burrard Street, Suite 510
Vancouver, British Columbia
V63 3A8
Tel: (604) 687-2153
Prospecting, Rock Geochemistry and Recon Geophysics
Work performed from May13, 2008 – December 31, 2008
Prepared By:
Dean Fraser, P.Geo. and Andy Thomas, MSc.
December 2008
ii
SUMMARY
During October 2006, Bayswater Uranium Corporation acquired and staked a total of
290 claims in the Makkovik River Area of the Central Mineral Belt of Labrador.
Through a Joint Venture deal with UCore Uranium Inc., an additional 539 claims were
combined under an agreement between the two companies. The Bayswater/UCore
Makkovik River property staked during 2006 accounted for a total of 829 claims covering
an area of 20,725 hectares. The Central Mineral Belt hosts numerous uranium deposits
and has become the focus of renewed exploration over the past several years.
Bayswater/UCore initially staked the grounds as it believed its exploration licenses had
potential to host economic uranium deposits of different geological styles, including the
world class IOCG and Rossing types.
As part of its 2007 exploration program, Bayswater/UCore commissioned NovaTem Inc.
based out of Mont Saint-Hilaire, Quebec to fly a high resolution helicopter-borne
radiometrics and magnetic survey over the entire J.V. land package. A total of 2491 line
kilometers of data was acquired over the J.V. claims as part of a larger survey
commissioned by Bayswater. Field work was carried out by a crew of eight prospectors
and two geologists during the period of August 05th to October 15th 2007. The airborne
survey proved very effective in identifying targets for ground follow-up. In total, twenty
nine priority targets were identified based in-house interpretation of the data. Numerous
lower priority targets also required ground investigation.
A total of 94 samples were collected during the 2007 program and submitted for multielement analysis at Activation Laboratories of Ancaster, Ontario. Results from the
survey were very encouraging and uranium enrichment was noted predominantly within
brecciated magnetite bearing granites, leucogranite and pegmatite veins. In addition,
assays show the presence of high rare earth element (REE) content with accompanying
gold in several areas. The 2007 program led to the discovery of three significant
uranium occurrences; the Makkovik River East, Makkovik River West and the CD
showings. The best results from grab samples taken from outcrop in all three areas
assayed better than 0.10% U3O8 and up to 0.14% U3O8. A detailed assessment report
of the 2007 program has been submitted to the Department of Natural Resources of
Newfoundland.
During 2008, the Company’s carried out a limited exploration program consisting
mainly of prospecting. A total of sixteen days of prospecting were completed. Field
work was carried out by a crew of two geologists and up to nine prospectors, during the
period of July 13th to September 21st 2008. Efforts were focused on the main mineralized
zones identified during the 2007 field season, namely the Makkovik River East and West
showing. Additional work was expanded between the two areas. In addition, a small
reconnaissance grid was established over the main showing at Makkovik River East.
Ground magnetometer, scintillometer, and a rock geochemical sampling surveys were
carried out over this grid. The CD showing was revisited but
iii
considered to be of lower priority therefore little attention was focused in this area.
A total of 45 samples were collected during the 2008 program and submitted for multielement analysis at Activation Laboratories in Ancaster, Ontario. Results from the
survey confirmed additional areas of uranium mineralization which require further
detailed work. The bulk of the work was concentrated in the Makkovik River East area,
which appears to contain the most promising mineralization. The best results from grab
samples collected in 2008 from outcrop, assayed up to 0.045% U3O8, and from float up
to 0.079% U3O8. The area is still currently considered to have potential to host a bulk
tonnage, low grade uranium deposit. Further work is warranted.
The following report describes the work performed during 2008. All data and maps are
appended to this report.
.
iv
TABLE OF CONTENTS
Page
SUMMARY ............................................................................................................................ ii
I. INTRODUCTION
Location and Access.........................................................................................................1
Physiography and Glaciation............................................................................................1
Property Summary License Status ..................................................................................1
Previous Exploration Work .............................................................................................3
II. GEOLOGY
Regional Geology.............................................................................................................5
Property Geology .............................................................................................................6
III. 2008 FIELD PROGRAM
Purpose .............................................................................................................................8
Exploration Methodology and Sampling .........................................................................8
Sample Preparation.........................................................................................................11
Prospecting Results ........................................................................................................11
Area between Makkovik River East and West showings ......................................13
Makkovik River West showing .............................................................................13
Makkovik River East showing...............................................................................14
IV. CONCLUSIONS AND RECOMMENDATIONS .......................................................18
V. REFERENCES .................................................................................................................19
VI. STATEMENT OF QUALIFICATIONS ......................................................................20
LIST OF FIGURES
Figure 1: Bayswater/Ucore Claims Location Map ...................................................................2
Figure 2: Regional Geology Map of Labrador .........................................................................9
Figure 3: Simplified Property Geology Map ..........................................................................10
Figure 4: Makkovik River Property Airborne U Radiometrics with Uranium Showings .....12
Figure 5: Makkovik River Property Airborne Magnetics with Uranium Showings...............13
Figure 5:6 Makkovik River East and West Showings Location Map ......................................14
Figure 6:7 Makkovik River East Recon Scintillometer Survey Map .......................................16
Figure 7:8 Makkovik River East Recon Magnetometer Survey Map.......................................17
v
LIST OF TABLES
Table 1: Current Bayswater/UCore Claims ...............................................................................3
Table 2: Average trace element composition of eight granitoid
samples from within the Bayswater/UCore J.V. area, compared with
peralkaline and calc alkaline granitoids and rhyolite from the Letitia
Lake area of central Labrador .....................................................................................7
LIST OF APPENDICES
Appendix A: Personnel, Contractors and Expenditures
Appendix B: 2008 Summary Rock Sample Database and Rock Sample Site Location Map
Appendix C: Activation Laboratories Assay sheets
Appendix D: Bayswater/UCore 2008 Claims Map
Bayswater/UCore J.V
Makkovik River Uranium Project
1
I. INTRODUCTION
Location and Access
The Bayswater/UCore Joint Venture mineral exploration licenses are located within the Central
Mineral Belt of Labrador and not far from the coastal communities of Postville and Makkovik.
The property is centered approximately 30 kilometers east-southeast of Postville and 30 kilometers
south-southwest of Makkovik (Figure 1).
The 2008 field exploration program was based out of the town of Postville. Sufficient
infrastructure and facilities exists in the community providing an excellent staging area for field
support and logistics. Access to Postville can be obtained by regular scheduled commercial twin
otter aircraft, or the less frequent coastal ferry service from Happy-Valley Goose Bay. Road
access is not available out of the community.
Access to the claims areas can be obtained by helicopter either from the coastal towns of Postville
or Makkovik. A fifteen to twenty minute helicopter fight either way is required to access the
center of the claims.
Physiography and Glaciation
All claims within the Bayswater/UCore project area are situated on rugged glaciated terrane of
moderate relief and elevation. Rocks generally form barren to sparsely vegetated rounded hills up
to 600 m in elevation. These are separated by wide boulder filled U-shaped valleys and locally
incised structurally controlled areas. Rolling hills dominate the exploration license with local
valleys and river beds more heavily forested. Boulder cover extends to the tops of and over many
of the ridges, forming fields which effectively reduce bedrock outcrop exposure in many areas,
especially the valleys, to nearly nothing. Abundant lakes and smaller ponds exist throughout the
project area.
Measurements throughout the project area, on glacial indicators such as striae, chattermarks, and
crag and tail features, yield weak evidence for early ice movement from the northwest or west, and
strong evidence for later movement from the southwest.
Property Summary License Status
The Bayswater/UCore Exploration Licenses at the writing of this report consists of 816 claims,
covering a total area of 20,400 hectares. It is expected that a reduction in the claims holdings will
occur during 2009. Table 1 summarizes the individual claim licenses held within the Bayswater/
UCore Joint Venture, all of which are currently held in good standing. A detailed claims location
map can be found in Appendix D of this report.
Bayswater/UCore J.V.
Figure 1: Bayswater/UCore Claims Location Map
2
3
License No.
No. of Claims
Work Due License No.
Date
No. of Claims Work Due Date
Bayswater Claims
012775M
71
012780M
72
012819M
4
012821M
6
012825M
3
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29,09
012777M
012818M
012820M
012822M
114
9
6
5
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
UCore Claims
012735M
37
012768M
160
012786M
14
012788M
6
012791M
4
012794M
34
012796M
3
012801M
53
012808M
16
012829M
10
012831M
1
Jan 28, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
012747M
012784M
012787M
012790M
012793M
012795M
012798M
012803M
012809M
012830M
012832M
30
46
26
20
8
12
14
16
14
1
1
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Jan 29, 09
Table 1: Current Bayswater/UCore Claims
Previous Exploration Work
Exploration for uranium and base metals in the Central Mineral Belt of Labrador (CMB) was first
begun in 1955 by Brinex. The first significant uranium showing was found by Walter Kitts in
1956, and was followed by a program of diamond drilling and underground development in 1957.
Work was suspended the following year, and nothing further was done with this showing until
1966.
In 1959, Lundberg Explorations Limited (Lundberg) carried out an airborne geophysical survey in
the Ugjoktok Bay area for Brinex. The objective of this survey was to explore for base metal
deposits. Numerous electromagnetic (EM) and coincident magnetic anomalies were detected
(Wilson, 1959). In general, these were grouped as follows:
(1) Conductors associated with altered peridotitic sills.
(2) Conductors located in areas underlain by greenstone terrains.
(3) Conductors located in areas underlain by granitic rocks, or granite-gneiss within
greenstone terrains.
(4) Conductors interpreted to be expressions of graphitic horizons, or pyritic schists within
the greenstone rocks.
(5) Conductors associated with lakes and ponds.
4
None of the conductors were thought to represent large sulphide bodies.
In 1963 and 1964, Brinex carried out reconnaissance geological mapping, prospecting, and lake
sediment and soil sampling geochemical surveys in the area of its Ugjoktok Concession. Brinex
detected a number of base metal (Ni, Cu, and Mo) anomalies, but no significant follow-up work
was reported (Bondar, 1963, Lee and Moghal, 1964, Earthrowl, 1964).
In 1966, Brinex and Metallgesellschaft A.G. (Metallgesellschaft), a German energy company,
formed a joint venture agreement to explore part of the lease containing the Kitts uranium deposit.
Metallgesellschaft subsequently transferred its interest to its wholly owned subsidiary,
Urangesellschaft Canada Limited (Urangesellschaft), with which the agreement continued. This
partnership resulted in the discovery of a number of uranium showings, including the Michelin
deposit (by prospector Leslie Michelin) in 1968, as well as the Gear, Inda, and Nash showings
during 1968 and 1969. All of these discoveries were made by follow-up ground spectrometer
surveys, on anomalies detected from airborne radiometric surveys.
During the 1970s, Brinex carried out further reconnaissance work in the CMB, as well as detailed
exploration on the Michelin deposit. This included a combined helicopter borne EM, magnetic,
and radiometric survey, within a large area outlined by Longitudes 53° 30’W to 54° 37’W, and
Latitudes 61° 00’N to 63° 00’N, by Sander Geophysics Limited (Sander). The objective of this
survey was to detect EM conductors that could be expressions of copper mineralization in the Seal
Lake area. A number of conductors were detected which were interpreted to represent graphitic
slates (Sander, 1971). Radiometric anomalies were detected to the south and east of Moran Lake,
where some uranium showings were known to occur. One of these anomalies “appears to represent
a uranium deposit” (Moran Lake deposit?). Strong radiometric anomalies were detected within the
Letitia Lake Group, and were generally characterized as being due to thorium. Sander (1971)
considered the “uranium channel radioactive anomalies in the extreme east and west parts of the
surveyed area, and the thorium anomalies in the Letitia Lake Formation as the best prospects
located during the survey”. In early 1971, Sander carried out further airborne combined EM,
magnetic and radiometric surveys in the Kaipokok Bay-Seal Lake area for Brinex. The purpose of
this survey was to map the surface distribution of radioactive materials within the area, and to
distinguish between potassium, uranium, and thorium sources. At least twenty-nine (29) EM
conductors and twenty-five (25) radiometric anomalies were detected (Goddard and Klein, 1971).
In 1977, Brinex and Canadian Nickel Exploration Company (Canico) carried out reconnaissance
geological mapping, and anomaly follow-up on the joint venture lands, which included the Seal
Lake and Moran Lake areas. A number of radioactive showings were discovered in the Boundary
Lake and Madsen Lake areas. These included radioactive boulders which returned values ranging
from 0.01% U3O8 to 0.095% U3O8 (Phipps, 1978). The Brinex-Canico joint venture also
discovered bedrock uranium occurrences, and carried out prospecting, ground geophysical (EM
and magnetometer) surveys, and limited diamond drill testing at Boiteau Lake and in the Green
Pond/Embee Pond area (Perry, 1980). These localities were visited during the ground portion of
Bayswater’s 2006 field exploration program.
In 1978, Brinex carried out further reconnaissance lake sediment geochemical surveys, and in
1979, an airborne radiometric survey in the Kaipokok River region. As a result, one prospect in
particular (J & B), and other mineral showings in general were found to be associated with felsic
rocks (Davidson, 1979).
5
In 1993, the Geological Survey of Canada (GSC) carried out a detailed helicopter supported lake
sediment and lake water geochemical survey, covering much of the current Bayswater mineral
lands.
Limited exploration for uranium had been documented since the Brinex era in the CMB, until
Altius Minerals Ltd. staked several of the known deposits including the Michelin in 2004. As a
result of the price increase in uranium, and interest in the economic mineral potential of the area,
the belt has been staked in its entirety and exploration is ongoing by numerous companies.
The current Bayswater/UCore claims group had not been explored during the most recent
exploration rush as a result of the lands being exempt from exploration while the Nunatsiavut
Government finalized their land claims. On October 31st, 2006 the ground was opened for
exploration and a staking rush occurred. Bayswater and UCore acquired 829 claims during this
rush. A detailed airborne survey and reconnaissance prospecting was initiated in 2007 that led to
the discovery of several uranium showings of interest; namely the Makkovik River East and West
showings. A detailed prospecting program was again performed during 2008 in and around these
previously identified targets and is the focus of this report.
II. GEOLOGY
Regional Geology
The area examined during the Bayswater/UCore Labrador Uranium Exploration Program covers a
small portion of the eastern part of the Central Mineral Belt (Figure 2). The CMB is situated within
close proximity to the intersections of the Nain, Churchill, Makkovik and Grenville structural
provinces. The Nain Province comprises mostly tonalitic to granodioritic gneisses, and variably
deformed granodioritic intrusive bodies with subordinate mafic volcanic/volcaniclastic rocks of
Archean age. A northeast trending 1 to 2 km wide mylonite zone forms the boundary between the
Nain and Makkovik provinces (Ermanovics, 1993).
The Makkovik Structural Province comprising the Kaipokok, Aillik, and Cape Harrison tectonic
domains, is a triangular wedge situated between the Nain province to the north, and Grenville
province to the south (Agnerian, 2006). Bedrock within this province consists of reworked
Archean Hopedale block gneisses, as well as granodioritic to granitic intrusive bodies, mafic to
felsic volcanic and volcaniclastic rocks, and metamorphic schistose equivalents varying in age
from Archean to Paleoproterozoic. The two main supracrustal rock sequences present are the
middle Proterozoic Moran Lake and Lower Aillik groups. The Kaipokok Bay shear zone (Figure
2) passes northeast below its namesake, defines the boundary between the Kaipokok and Aillik
tectonic domains, and marks the southern limit of known Archean crust in the Makkovik Province
(Agnerian, 2006). The Bayswater/UCore claims lie along the southeastern boundary between the
Makkovik and Grenville structural provinces.
The boundary between the Grenville and Makkovik structural provinces is a northeast to east-west
trending belt of arcuate en echelon moderate angle reverse, and/or lobate thrust faults and nappes.
The Bayswater/UCore claims straddle rocks along the noses of the most easterly regional thrust
lobes, in the vicinity of the headwaters of the Makkovik River near the Labrador Sea coast. Major
re-entrants along limbs of these regional thrust lobes are found in the vicinity of the Smallwood
6
Reservoir, and northwest of Lake Melville along the Pocketknife Lake Fault (Figure 2). Limited
Grenvillian folding and tectonism may also be present within Makkovik Province rocks north of
this belt. Apart from the Grenvillian deformation, major middle to late Paleoproterozoic volcanic
centers of the Upper Aillik and Bruce River Groups (Figure 2), the Grenville Province in this
region is characterized by para- and orthogneisses, as well as deformed granite, granodiorite and
diorite. Unique to this region are several deformed gabbronoritic dykes of different generations
and orientations, one of which forms a prominent discontinuous northeast trending ridge traceable
for many kilometers through Bayswater’s southeast claim block. Additional unusual (in part
metasedimentary), and previously unmapped rock types, were found in this thrust belt during the
course of the 2006 exploration.
Rocks of the Grenville, Nain and Makkovik Structural Provinces, are separated from those of the
Churchill Province to the west by both the north-south trending Pocketknife Fault, and eastern
intrusive contact of the Harp Lake Anorthosite. Both of these features are emphasized by an
accompanying regional magnetic lineament. The Nain-Churchill Province boundary passes
through or close to the western edge of Bayswater’s Northwest claims block, and is marked mainly
by a change of bedrock structural trends from northeast-southwest to north-south.
Property Geology
The Bayswater/UCore exploration licenses lie within the Aillik Domain of the Makkovik structural
province. The property lies across a salient of regional lobate thrusts partly defining the northern
boundary of the Grenville Front in Eastern Labrador, which in this area manifests itself mainly as a
foreland thrust belt. The claims are predominantly underlain by proterozoic granitic and mafic
intrusive units, containing local slivers of similar aged volcanic rocks that host many of the
uranium deposits within the Central Mineral Belt of Labrador. A brief summary of the property
geology is given below, and Figure 3 provides a simplified geological map of the area underlying
the Bayswater/UCore exploration licenses. No detailed geological mapping has been initiated
during 2008.
Exposure is mixed within the rocks of the claims block. The northern half of the property is
characterized by barren to sparsely till covered hills, whose summits contain abundant bedrock
outcrops. Bedrock in the remaining southern half of the area is extensively boulder covered and
outcrops are rare. Exposed bedrock and boulders within the Bayswater/UCore JV property
comprise two main rock types. Medium to coarse grained reddish-pink to buff coloured
equigranular magnetite-rich granite/granodiorite and pegmatite. Uranium mineralization is
commonly associated with brecciated and hematitic variants of the magnetite bearing granites.
Veins of coarse grained white pegmatite, associated with uranium mineralization, have also been
identified within the area. The same lithologies can also be found in most of the boulder cover. The
granitic rocks may exhibit both igneous and metamorphic textures. Pegmatite observed in boulders
appears undeformed. A strong airborne magnetic anomaly is directly associated with the
granite/granodiorite unit, as are a number of related airborne radiometric anomalies (Figures 4, 5).
Fluorite is present sporadically throughout exposed bedrock areas in the granitoid rocks.
Hematization and brecciation of the granitic rocks was also reported at several localities.
7
There are indications from trace element analyses on assayed samples of both bedrock and
boulders, of a significant and widespread Rare Earth Element (REE) enrichment pattern. The
average trace element content of eight selected granite bedrock samples from the claim block is
compared with corresponding averages of rocks collected from the central Labrador Letitia Lake
peralkaline volcanic centre. Table 2 below, lists the average trace element analyses for fourteen
Arc Lake Intrusive Suite peralkaline granites, ten Letitia Lake Group peralkaline rhyolites, and
twenty-two calc-alkaine monzonitic to granitic rocks from the spatially associated North Pole
Brook Intrusive Suite. The Bayswater/UCore samples exhibit evidence of either a peralkaline
affinity or alteration resulting in preferential REE enrichment or both. The key indicator trace
elements Zn, Sr, Y, Zr, Nb, Ba, and La show a combined enrichment pattern characteristic of
peralkaline rocks, although some are inordinately high and may indicate instead that the chemistry
of these rocks has been altered. Uranium, thorium, and yttrium trace element content is excessive
for peralkaline rocks, and may reflect the effects of some sort of alteration process. These rocks
have undergone Grenvillian tectonism and metamorphism, as well as other possible emplacement
and/or post emplacement, pre Grenvillian events. Trace element data suggests that there may be
remnants of a previously unrecognized pre-Grenville peralkaline volcanic centre, present in the
vicinity of the Bayswater/UCore J.V. ground.
Bayswater
Arc L.
(Grt. 8) (Per. Grt. 14)
Letitia L.
(Per. Rhy, 10)
North Pole Brook Intrusive Suite
(Qtz Monz/Grdt. 18) (Monz. 4)
Be
12
10
7
V
5
0
5
85
Cr
12
11
11
14
Ni
1
30
28
43
Cu
17
6
9
10
*Zn
213
151
127
49
Ga
51
29
25
20
Rb
171
258
214
135
*Sr
28
21
29
391
*Y
851
111
132
34
*Zr 1734
1087
1061
205
*Nb 252
78
67
15
*Ba 133
70
162
1151
*La
76
121
129
39
Pb
142
39
32
20
Ce
227
158
165
123
F
252
638
852
Th 124
21
19
10
U
289
5
4
2
* Key indicator trace elements for a peralkaline signature
127
9
29
9
70
21
86
919
29
136
6
1814
27
7
130
1010
3
1
Table: 2 Average trace element composition of eight granitoid samples from within the
Bayswater/UCore J.V. area, compared with peralkaline and calc alkaline granitoids and
rhyolite from the Letitia Lake area of central Labrador.
8
All bedrock within the Bayswater/UCore J.V. area has been affected by Grenvillian compression
from the south. Reverse and thrust faults have resulted in emplacement of rocks from the south,
with the granitoids in the area now stacked into successive overriding and/or overlying tectonic
sheets. The granitic rocks are massive or foliated, but may also exhibit localized cataclastic,
mylonitic, and brecciated textures. The number, type, and age of igneous units within the
Bayswater/UCore J.V area are not presently well known, nor well documented.
III. 2008 FIELD PROGRAM
Purpose
The Bayswater/UCore 2008 field program was carried out with the expressed purpose of
continuing grassroots exploration for uranium potential within the J.V. land claims. The 2008
program focused on the key areas identified during the 2007 exploration program. As the
proposed exploration program for the project was small, only priority areas were explored. The
Makkovik River East and West showings along with area between these two occurrences were
targeted for the bulk of the prospecting program. The potential for a low grade, bulk tonnage
uranium deposit is thought to exist in the area and was the primary focus of the Company’s
exploration efforts. Particular attention was given to geophysical data acquired from airborne
magnetics and radiometrics surveys flown during 2007.
Exploration Methodology and Sampling
The 2008 field program consisted of detailed prospecting based on continued in-house processing
and interpretation of the airborne survey carried out in 2007. Results from that survey originally
delineated twenty nine primary targets, and numerous secondary targets of interest for ground
follow-up. For additional information on these targets, refer to the first year assessment report for
this project. Only the highest priority targets were prospected during 2008. In addition, a small
reconnaissance grid was established near the northeastern boundary of the Bayswater/UCore
claims, over an area of anomalously high radioactivity designated the Makkovik River East
showing. A survey of the grid was carried out and included ground magnetometer, scintillometer,
and geological sampling components. The gridding was performed as a prelude to a proposed
drilling program in the area. This program was abandoned at the final stage of planning and will
be performed at a later date. A group of nine prospectors and two geologists carried out ground
follow up on all claim blocks during the first half of the field season. Four prospectors and two
geologists worked the ground during the second half of the season. A total of sixteen days of
prospecting were completed during 2008. These personnel were given specific GPS coordinates
with which to locate targets of interest, and helicopters were used to emplace ground traverses or
to make spot landings as required. Rocks having scintillometer readings equal to or greater than
1000 CPS were sampled wherever possible.
All personnel carried either Exploranium GR110 hand held scintillometers, or an Exploranium
GR135 hand held spectrometer (three of which was available for use as required). Both bedrock
and boulders were sampled in the usual manner by hammer or maul, fist sized or larger rocks
being the norm. Samples were labeled, dried whenever possible, emplaced in plastic bags, and kept
under lock and key while awaiting bi-monthly shipment to Activation Laboratories Ltd. for assay.
Figure 2: Regional Geological Map of Labrador
9
Figure 3: Simplified Property Geology Map
10
11
A total of 45 samples were collected and submitted for multi-element analysis. All copies of the
original assay sheets are appended to this report. A printout of the summary rock sample database
is also included as Appendix B. All samples were analysed for uranium by both Mass
Spectrometer and Neutron Activation delayed neutron counting techniques. Quality Assurance/
Quality Control (QA/QC) work was performed by Bayswater to insure data quality. A suite of
commercial uranium rock standards were submitted by Bayswater at pre-determined intervals for
in-house quality control. Activation Laboratories ensured reproducibility of results by the addition
of internal blanks and duplicates. Results of the QA/QC work indicate all assays were in the
permitted range of error. The following summarizes sample preparation and assay techniques
performed by Activation Labs:
Sample Preparation
The rock sample submitted is dried at 60 degrees C, and crushed using a TM Engineering
Terminator crusher to at least 85% -10 mesh. The sample is then riffle split, and an aliquot of at
least 100 grams is pulverized in a mild steel ring mill to at least 95% -150 mesh (Code RX2-Crush
and mill). Finally it is analysed utilizing one or more of the following techniques:
(1) Uranium by Delayed Neutron Counting-DNC (Code 5D-U DNC)
A 1 gram sample is doubly encapsulated in a polyethelene vial. Samples are sealed
and are irradiated serially in a computer controlled vial transfer system. The sample is sent
automatically to a delayed neutron counter, and delayed neutrons are thermalized and
counted by an array of BF3 detectors. Count rates are compared to a standard calibration
made from certified reference materials. The range of analysis for this method is 0.1 ppm to
1% U.
(2) Assay by XRF (Code 8-U)
A 0.5 gram sample is subjected to loss on ignition at 1050 degrees C. The sample is
then mixed with a combination of lithium metaborate/tetraborate, and fused in platinum
crucibles using a Claisse automatic fluxer. The molten liquid is poured into platinum dishes
and allowed to cool. The fused glass disks are placed into a Panalytical PW-2400
wavelenth dispersive XRF unit using an autosampler. Data is reduced using Philips Super
Q software, and compared to a standard calibration developed from multiple certified
international reference materials. Range of the method is 0.005 to 10%.
A list of elements and detection limits can be found at www.actlabs.com.
Prospecting Results
Reconnaissance prospecting of priority radiometric targets during 2007 led to the discovery of
three uranium mineralized areas. These are termed the Makkovik River East, Makkovik River
West, and the CD showings (see Figure 4). During the early part of the 2008 field season all three
areas were revisited. The CD showing mineralization was found to be related to very sparse and
narrow biotite rich shears and thus further attention was not placed on this area. The bulk of the
exploration was focused in and around the areas of the Makkovik River East and West showings.
Figure 4: Makkovik River Property Airborne U Radiometerics with Uranium Showings Map
12
Figure 5: Makkovik River Property Airborne Magnetics with Uranium Showings Map
13
14
These showings are located in the northern portion of the J.V. exploration license (Figure 4).
Results obtained from the program were successful in delineating additional outcrop and boulder
showings of interest in the area. Detailed geological work and regional geological mapping were
not undertaken on any of the claims within this block. Appendix B provides a summary database
with accompanying Rock Sample Site Location map for the 45 rock samples collected during the
2008 field season. A complete digital rock sample database has also been appended. The
following provides a description of results from the areas prospected.
Area between Makkovik River East and West Showings
Although uranium mineralization was found previously in both the Makkovik River East and West
showings, the area between them received only cursory examination and therefore was prospected
more thoroughly during the 2008 exploration program. A number of mineralized rock samples
were collected from this area (see Appendix B), four of which came from outcrop, the remainder
from boulders, float or frost heaves. The best three outcrop samples were collected from white,
coarse-grained magnetite-bearing granite exposures located approximately 2.2 km southeast of the
Makkovik River West showings. The ID numbers for these samples are 50110, 50109 and 50602.
These samples give scintillometer readings of 3000cps, 2400cps and 2000cps, and yield assays of
381ppm, 247ppm and 13ppm U respectively. All three samples assayed greater than 200ppm Th,
and exhibit REE element enrichment. The first sample is enriched in Zr (2090ppm), Nb (1023ppm)
and Yb (126ppm), the second in Ce (174ppm) and Nd (204ppm) and the third in La (514ppm), Ce
(1270ppm) and Nd (477ppm). The third sample also contained 316ppm Zn. In addition,
anomalously high contents of Y, Er, and Gd are also present in all three samples.
Boulders and float accounted for 33 of the samples collected from the area between the Makkovik
River East and West showings. Similarly to those from outcrop, these samples comprised white
coarse-grained magnetite-bearing granite or white to pink pegmatite. Scintillometer readings
ranging from 1000cps to 6500cps were obtained, but not all radioactive samples returned assays
with anomalous uranium values. Assays from these rocks indicated uranium contents between a
minimum of less than 5ppm, and maximum of 513ppm. Also in common with outcrop, 8 boulder
and float samples returned assays of greater than 200ppm Th. REE enrichment in Zr (up to
2090ppm), Nb (up to 284ppm), Yb (up to 144ppm), Ce (up to 175ppm) and Nd (up to 204ppm) is
common within many boulder and float samples (Appendix B). Several boulders and float are
preferentially enriched in Y, Er, Dy and Gd. Additional prospecting and field work is warranted in
this area.
Makkovik River West showing
The Makkovik River West Showing found in 2007 is characterized by a moderately radioactive
airborne anomaly that measures 1.0 kilometer long by 500 meters in width (Figure 4). The
Makkovik River West showing is located within an extensive zone of low magnetic relief
indicating the presence of a potentially large alteration system related to regional thrusting, or
differing rock units from what are mapped regionally by Government geologists (Figure 5).
Several traverses carried out during 2008 in the vicinity of the showing did not result in any new
finds, but did confirm further the previously discovered mineralization, condensed as follows from
the First Year Assessment Report. The zone occurs 3.0km to the west of the Makkovik River East
15
showing, is 1.7km long by 1.2km wide and trends west to east. The area is smaller than and
mineralization is not as intense as that in the East showing, however it occurs within identical rock
types. Scintillometer readings on bedrock vary from 700cps to 9999cps and from 1800cps to
9800cps on boulders. The highest uranium assay obtained on bedrock samples from this showing
returned values of 127ppm. Of the boulders sampled, three returned assay values for uranium of
136ppm, 248ppm and 960ppm. Thorium is commonly present in amounts in excess of 200ppm in
all rocks from the area. Bedrock and boulders in the Makkovik River West showing exhibit a
similar rare element enrichment pattern to that seen in the East showing, with the highest assay
values returned from bedrock being 1220ppm Zr, 880ppm Ce, 407ppm Nd, 324ppm La, 234ppm
Y, and 103ppm Pr. For boulders, the highest assay values returned 2360ppm Zr, 1420ppm Y,
>500ppm Nb, 326ppm Ce, 285ppm Nd, 201ppm Dy, >200ppm Yb, 183ppm Er, 158ppm La,
154ppm Gd, 90ppm Hf and 66ppm Ho.
Makkovik River East showing
Based on data collected from the airborne radiometric survey carried out in 2007, the Makkovik
River East Showing is marked by a well defined 400 meter long by 200 meter wide zone of
elevated radioactivity (Figure 5). Two additional radiometric anomalies were also identified in
close proximity to that of the showing. Airborne magnetic data indicates the zone is located in an
area of low magnetic response that flanks an irregularly shaped local magnetic high, directly to the
east and south of an arcuate linear magnetic high to the west. The showing underwent initial
prospecting in 2007 and with the encouraging results obtained from grab sample assays (see First
Year JV Assessment Report) it was decided to establish a small reconnaissance grid during the
2008 field program. A 300m long baseline, with 200m long cross lines spaced every 20m, was laid
in on a true bearing of 125 degrees. The area covered by the grid was then subjected to both
ground magnetometer and scintillometer surveys. Results from the recon survey showed an area
of elevated scintillometer readings between line 100W and 500W. This corresponds to the area of
the main showing (Figures 6 and 7). The limited total field magnetic data makes it difficult to
perform a reasonable interpretation. No direct correlation or valid interpretations can be made
other than noting an arcuate magnetic high response flanked by magnetic lows to the north and
south runs through the center of the grid area. Additional work is required to aid in a better
interpretation of the data.
Work within the grid area during 2008 resulted in the gathering of 8 uranium mineralized samples
additional to those collected during 2007. Unfortunately all of these were taken from boulders and
float. These boulders comprise both magnetite-rich granite/granodiorite and pegmatite.
Scintillometer values of sampled material ranged from 1400cps to 6000cps and yielded uranium
assay values of 161ppm to 674ppm U (see Appendix B). Five of the eight samples returned assays
over the detection limit of 200ppm Th. Six of the samples exhibit the REE enrichment found
within other rocks in the area. Very strong REE enrichment patterns occur in Zr (543 to
>5000ppm), Nb (117 to >500ppm), Yb (90 to >200ppm), Ce (214 to 226ppm) and Nd (122 to
231ppm). These samples also exhibit higher than normal enrichment in Y, Er and other REE
elements. The sample that contained >5000ppm Zr also contained 1430ppm Y, 482ppm Zn,
283ppm Dy, 259ppm Er, 178ppm Gd, 154ppm Hf and >100ppm Sm.
Both bedrock and boulders in the Makkovik River East showing are unusual in chemistry. Many
Bayswater/UCore J.V
Figure 6: Makkovik River East and West Showings Location Map
16
Bayswater/UCore J.V
Figure 7: Makkovik River East Recon Scintillometer Survey Map
17
Figure 8: Makkovik River East Recon Magnetometer Survey Map
18
19
of the trace elements listed above occur only rarely in normal everyday rocks, and then in very
small amounts. They are present in Makkovik River granitoids in amounts in excess of ten times
what they normally would be, where these elements do occur at all. In addition significant low
level uranium and thorium mineralization is widespread. This indicates that within the Makkovik
River East showing (and probably the surrounding area) there is a sizeable volume of very
unusual, possibly altered, but definitely mineralized rock type present. Additional detailed work
including reconnaissance drilling is warranted in this area.
IV. CONCLUSIONS AND RECOMMENDATIONS
The Makkovik River area of the Bayswater/UCore Joint Venture claim block is underlain by a
sizeable volume of Precambrian granitic and pegmatitic rocks, containing uranium, thorium and
Rare Earth Element enriched mineralization. Although of a low grade, this mineralization is
widespread and distributed within large plutonic bodies. It may be primary in nature and associated
with emplacement of these bodies, or it may be due to secondary alteration, or a combination of
both processes. The region has undergone several periods of Precambrian orogenesis, and
mineralization may have originated with associated tectonic and metamorphic events. The REE
enrichment may be due to the presence of one or more peralkaline intrusive events, which have
previously gone unrecognized.
It is recommended that rocks within the Bayswater/UCore JV claim blocks be examined in more
detail, especially the northern part around the Makkovik River showings, in order to better
ascertain their potential for a low grade, large tonnage uranium deposit. The REE deposit potential
of the area’s rocks should also receive greater consideration. All the ground in the vicinity of the
Makkovik River showings, should be examined in more detail, and at least subjected to a basic
geological mapping program as well as additional bedrock geochemical sampling. A
reconnaissance diamond drilling program should be carried out on mineralized bedrock outcrops
within the Makkovik River East grid.
20
V. REFERENCES
Agnerian, H., 2006, Technical Report on The Central Labrador Uranium Project,
Newfoundland and Labrador: N143-101 Report Prepared for Bayswater Uranium
Corporation by Roscoe Postle Associates Inc., March 2006.
Bondar, W.F., 1963, Geochemical Exploration, Ugjoktok Area, Labrador 1963: Brinex
Internal Company Report.
Davidson, G.I., 1979, Brinex Limited, Labrador Uranium, Areas A and B, Airborne
Radiometric Survey, North Kaipokok River Region Area B, Labrador: Brinex Internal
Company Report (P79010), December 1979.
Earthrowl, J.A., 1964, Final Report, Cliffs-Brinex Joint Area, Ugjoktok Concession,
Labrador: Brinex Internal Company Report, September 18, 1964.
Ermanovics, I., 1993, Geology of the Hopedale Block, Southern Nain Province, and the
Adjacent Proterozoic Terranes, Labrador, Newfoundland: Geological Survey of Canada
Memoir 431, 1993.
Goddard, P. and Klein, J., 1971, Report on Airborne Geophysical Surveys in the Kaipokok
Bay-Seal Lake Area, Labrador, on Behalf of British
Lee, S.L. and Moghal, M.Y., 1964, Geochemistry Laboratory Report 1964: Brinex Internal
Company Report.
Perry, J., 1980, Annual Exploration Report 1980, June 23-August 25, Canico-Brinex Joint
Venture, Moran Lake Area, Labrador, The Makkovik Area Principle Agreement (Act of
1953): Canadian Nickel Company Ltd. Internal Report, October 1980.
Phipps, D., 1978, Canico-Brinex Joint Venture, Labrador, Exploration Report 1977:
Canadian Nickel Company (Canico) Internal Company Report, Copper Cliff, Ontario,
January 1978.
Sander, G.W., 1971, Report on the Helicopter Borne Geophysical Survey on Behalf of
British Newfoundland Exploration Limited in the Ten Mile Lake, Seal Lake and Moran
Lake Areas of Labrador, Approximately 54oN 62oW: Report by Sander Geophysics
Limited for Brinex, Ottawa, April 15, 1971.
Wilson, B.T., 1959, Report on Airborne Geophysical Survey of the
Ugjoktok Bay Area, Labrador, for British Newfoundland Exploration Limited: Report by
Lundberg Exploration Limited for Brinex, August 10, 1959.
Wilton, H.C., 1996, Metallogeny of the Central Mineral Belt and Adjacent Archean
Basement, Labrador: Government of Newfoundland and Labrador, Department of Mines
and Energy, Geological Survey, Mineral Resource Report 8, St. John’s, Newfoundland,
1996.
22
I, Andre Thomas, Consulting Geologist of 116 Lawrence Pond Road E., Upper Gullies,
Newfoundland, Canada HEREBY CERTIFY THAT:
2) I am a graduate of both the University of Waterloo with a B. Sc. Degree in Earth Science
(1974), and the University of Western Ontario with a M. Sc. Degree in Geology, (1978).
2) Continuously from 1970 to 1995 and occasionally up to 2001, I was actively employed as a
geologist/geological technician in provincial government survey work, the mineral exploration
industry, and university research in various locations within Canada and Australia.
3) I have been engaged by Bayswater Uranium Corporation to act as Senior Project Geologist for
the company’s Central Mineral Belt Uranium Project located in Labrador, Canada.
4) I do hold a stock option with the company.
5) I am registered as a Professional Geoscientist with the Association of Professional Engineers
& Geoscientists of Newfoundland, but that registration is presently dues expired.
6) I approve of this report being used for any lawful purpose and filing requirements as may be
required by Bayswater Uranium Corp...
Dated at St. John’s, Newfoundland, Canada this 19th day of December 2008.
_____________________
Andre Thomas, B. Sc (E. Science), M. Sc (Geology)
APPENDIX A
(Personnel, Contractors and Expenditures)
PERSONNEL, CONTRACTORS AND EXPENDITURES
PERSONNEL
R. Dean Fraser – Project Manager –Bayswater Uranium Corp.
26 Blue River Place, St. John’s, NL
A1E 6C3
Andre Thomas – Senior Project Geologist – Bayswater Uranium Corp.
116 Lawrence Pond Road E., Upper Gullies, NL
A1X 4C6
Colin Finkbinder – Project Geologist – Bayswater Uranium Corp.
Vancouver, British Columbia
Calvin Crocker – Logistics Manager – Bayswater Uranium Corp.
Benton, Newfoundland
Bradford Jacque, Prospector – Bayswater Uranium Corp
General Delivery, Makkovik, Labrador
Robert Edmunds, Prospector – Bayswater Uranium Corp
General Delivery, Postville, Labrador
Rick Edmunds, Prospector – Bayswater Uranium Corp
General Delivery, Postville, Labrador
Lewis Standing, Prospector – Bayswater Uranium Corp
Burgeo, Newfoundland
William Ward, Prospector – Bayswater Uranium Corp
Port Hope Simpson, Labrador
Harvey Kippenchuck, Prospector – Bayswater Uranium Corp
Port Hope Simpson, Labrador
Dan Jacobs, Prospector – Champion Exploration
Westport, Newfoundland
Ken Lewis, Prospector – Champion Exploration
Baie Verte, Newfoundland
CONTRACTORS
Northern Air Support
Kelowna International Airport
6285 Airport Way
Kelowna, British Columbia
V1V 1S1
Tel: 250-765-0100
Universal Helicopters – Helicopter Contractor
P.O. Box 29, Station C
Happy Valley - Goose Bay, Labrador
A0P 1C0
Tel: (709) 896-2541
RDF Consulting Ltd.
26 Blue River Place
St. John’s, NL
A1E 6C3
Tel: (709) 747-1648
Activation Laboratories Ltd. – Analytical Services Contractor
1336 Sandhill Drive,
Ancaster, Ontario
L9G 4V5
Tel: (905) 648-9611
TOTAL EXPENDITURES AND DISTRIBUTION BY LICENSE NUMBER
SUMMARY OF
BAYSWATER/UCORE MAKKOVIK RIVER PROJECT EXPENDITURES
(January 1 to December 31, 2008)
Consultants and Employees
Project Manager (Including research/geophys interp– 10 days x $500/day) 5,000.00
Senior Project Geologist (6 days x $425/day)
2,550.00
Geologist (16 days x $350/day)
5,600.00
Prospectors 16 Days x 11 Prospectors = 176 man days x $350/day
61,600.00
Logistics Manager (Fuel, sample shipment, food -16 days x $400/day)
6,400.00
Executive Visit (George Leary/Vic Tanaka)
2,680.00
Pilot (16 days)
Food and Accommodations
Accommodations (233 man days x $40/person)
Meals (233 man days x $60/day)
9,320.00
13,980.00
Helicopter/Fixed Wing Support
Flying (22 hours x $1680/hr)
Fuel (22 drums x 205L x $2.30/L)
1 Aircraft Charter (NorthWind Aviation)
36,960.00
10,373.00
1,192.32
Travel
Airfare – (9 Prospectors x 1 way)
5,467.03
Geochemical Analysis
Analyses (Assay– 46 samples@$46.80/sample)
2,152.80
Ground Geophysics
1 Recon Mag/scint Survey (1 day @ $400/day)
400.00
Maps and Final Report
Project Manager (5 days x $500/day)
Senior Project Geologist (6 days x $425/day)
Maps
2,500.00
2,550.00
360.00
Sub-total………… $169,085.15
Overhead Charges (15%)
$ 25,362.77
Total…………… $194,447.92
License No.
Bayswater
Claims
012775M
012780M
012819M
012821M
012825M
UCore
Claims
012735M
012768M
012786M
012788M
012791M
012794M
012796M
012801M
012808M
012829M
012831M
012767M
# of claims
$Totals Spent
License No.
# of claims $ Totals Spent
71
72
4
6
3
0
0
5,074.72
0
5,338.76
012777M
012818M
012820M
012822M
114
9
6
5
0
11,418.12
7,612.08
0
37
160
14
6
4
34
3
53
16
10
1
8
0
0
0
0
0
58,435.12
3,806.04
0
0
0
0
0
012747M
012784M
012787M
012790M
012793M
012795M
012798M
012803M
012809M
012830M
012832M
012887M
30
46
26
20
8
12
14
16
14
1
1
5
0
0
32,985.68
25,373.60
10,149.44
15,224.16
17,761.52
0
0
0
1,268.68
0
Total:
$194,447.92
APPENDIX B
2008 Summary Rock Sample Database
And Rock Sample Site Location Map
BAYSWATER URANIUM CORP
Summary Rock Sample Database (Makkovik R.)
Sample #
ZONE 21
49628
49902
49904
49905
50001
50007
50101
50102
50103
50104
50105
50106
50107
50108
50109
50110
50111
50112
50113
50114
50120
50201
50202
50302
50402
50403
50404
50405
50406
50407
50408
UTM_E
346563
354038
350977
347389
352374
353983
351456
351212
351131
351120
351139
351141
351109
351137
347725
347506
351741
351994
352027
352136
353961
353984
354097
351163
351178
351397
351392
351621
351735
351832
352602
UTM_N
6085372
6082853
6081685
6082006
6082376
6082998
6083385
6083172
6083026
6082892
6082990
6083034
6083055
6083084
6083565
6083006
6083545
6083538
6083528
6083526
6082885
6082853
6082961
6081555
6083205
6083343
6083343
6083473
6083539
6083491
6083509
Type
Boulder
float
?
O/C
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
O/C
O/C
boulder
boulder
boulder
boulder
boulder
Boulder
Boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
Total CPS
1400
5800
2000
2000
1800
2500
1200
5000
2100
1000
1400
1400
2500
1100
2400
3000
2500
2100
1100
2700
1700
6000
2200
6542
2250
2700
2900
1100
1340
1300
1500
U
U308
U
U308
Th
Zr
Cu
Pb
Zn
Mo
Nb
La
Ce
Nd
Dy
Yb
ppm
%
ppm
%
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
0.1
0.005
0.1
0.001
0.1
1
0.2
0.5
0.2
0.1
0.1
0.1
0.1
0.1
0.1
0.1
TD-MS FUS-XRF
DNC
DNC TD-MS TD-MS TD-MS
TD-MS
TD-MS TD-MS TD-MS TD-MS TD-MS TD-MS TD-MS
TD-MS
63.2
63.1
0.007
626
674
0.079
16.1
172
3.8
43.5
28.1
1.3
11.5
47.6
90
30.3
2.9
2.9
> 200 > 5000
4.3
230
482
1
> 500
41.8
214
231
283
> 200
195
205
0.024
51.3
244
22.7
161
29.8
1.3
36.1
47.7
127
67.7
19.1
10.6
32.4
33.8
0.004
83.1
379
1.4
13.1
19.1
0.4
103
35.9
70.5
32.5
20.4
19
48.6
51.7
0.006
43.8
549
4
21.8
16.3
0.2
28.4
10.3
26.9
10.4
5.3
18.3
297
314
0.037
> 200
2110
1.7
121
308
5.2
181
98.5
226
122
87.6
115
9.5
9.6
0.001
10
21
46.5
14.4
13.7
0.4
8.3
1.2
3.6
3
2.3
1.8
60.9
66.2
0.008
> 200
257
4.7
107
72.7
0.9
60.5
24.2
54.5
31.7
32.8
25.9
100
100
0.012
161
174
4.9
59.6
55
0.4
63.5
3.3
12.6
18.3
34.4
37.4
169
173
0.02
> 200
1270
13.4
98.8
244
0.9
284
34.4
142
123
157
144
54.2
53.2
0.006
141
45
2.8
18.2
48.9
0.3
102
2
10.4
18.8
37.8
30.6
61.4
64.8
0.008
123
82
9.7
25.8
38.9
0.4
57.6
1.5
7
11.5
22.3
24.1
78.5
90
0.011
> 200
434
1.5
28.4
38
0.6
57.9
1.9
8.7
14.8
30.3
33.1
26.2
28.5
0.003
46.4
69
5.2
16.6
21.8
0.5
21.3
7.1
17.3
10.2
7.3
8.6
252
247
0.029
> 200
473
4.3
82.3
169
0.3
4.9
55.3
174
204
81
44.2
388
381
0.045
> 200
2090
87.7
104
82
0.3
102
6.5
32.1
39.3
70
126
142
153
0.018
> 200
737
3.9
39.6
25.8
0.4
58
3.5
16
29.9
74.3
90.8
148
144
0.017
> 200
366
5.4
98.9
31.9
< 0.1
9.1
1.6
10.8
24.8
55.8
54.2
23.4
17.6
0.002
51.6
22
2
16.3
12.3
< 0.1
30.5
0.5
2.2
4.2
11.3
10.7
4.7
3.6 < 0.001
51.5
391
5.8
28
74.9
2.6
10
56.8
127
53.6
9.1
6.1
191
194
0.023
175
343
4.1
102
174
0.6
87.7
44.8
109
50.1
44.3
62.5
222
247
0.029
> 200
1600
2.8
171
131
1.8
117
25.6
98.5
72.2
89.4
104
168
189
0.022
> 200
2200
1.9
153
74.9
0.6
> 500
5.1
26.8
24.7
60.7
90.5
16.9
513
533
0.063
50.6
850
5.3
177
110
0.1
52.9
109
175
80.2
17.1
75.2
59.9
0.007
66.7
151
4.2
30
23.1
0.3
10
1.1
4.1
7
16.3
16
160
143
0.017
> 200
484
3.2
98.3
68.2
0.2
15.9
4.1
15.8
24.6
47.8
41.7
56.5
44.3
0.005
93.5
43
2.6
48.5
41.4
0.1
11.3
3.1
10.6
10.7
9.6
7.6
62.3
34
0.004
102
40
1.4
29.6
22.7
0.2
45.5
2
7.3
9.9
14.9
13.3
64.8
49.5
0.006
76.2
456
2.7
20.6
30.7
0.3
46
1.1
4.7
6.5
16
18
22.5
20
0.002
14.7
8
1.9
19
14.6
0.1
43.4
2.2
7.1
7.4
14.3
14.1
62.9
46.7
0.006
106
26
1.9
26.6
8.6
< 0.1
14.3
0.9
5.6
12.9
34.7
34.1
50501
50502
50503
50504
50505
50506
50507
50508
50509
50510
50601
50602
50701
50702
50801
351612
351368
351221
351145
351145
351061
351091
351096
351106
351157
347799
347570
353953
353994
353958
6083607
6083315
6083177
6083082
6082904
6082948
6083048
6083069
6083100
6083092
6083602
6083247
6082978
6082978
6082833
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
boulder
O/C
float
float
boulder
1378
1630
2986
2130
2532
1724
1549
1653
1275
1642
1720
2000
1800
1800
1420
34.9
27.9
0.003
69.4
36
2.6
56.4
52.5
0.9
8.2
14.5
41.3
25.2
13.4
33.9
25.1
0.003
60
6
2.2
27.2
31.3
0.3
14.4
0.8
2.8
3.6
7.4
21.4
5.8
54.4
62.8
0.007
157
75
1.6
36.4
10.9
0.1
11.6
14.2
32.2
16.7
12.3
11.9
105
88.9
0.01
144
405
7.7
40
28.4
0.3
27.8
8
21.4
16.5
20
36.1
149
165
0.02
> 200
190
3.2
58.6
409
< 0.1
90.9
20.6
77.2
99.7
147
140
148
163
0.019
> 200
318
2.5
56.7
89.5
0.8
42.4
21.1
81.1
83.5
101
99.5
124
103
0.012
191
108
3.6
53
37.4
0.4
36.4
14.9
36.8
26.5
19.3
17
80.2
63.7
0.008
98.8
211
2
33.1
69.9
0.2
181
1.4
6
6.8
10
13.3
61.9
50.5
0.006
80.1
403
2.6
28.9
25.7
0.3
70
2.4
6.3
7.4
10
16.3
116
96.2
0.011
128
682
2.2
42.3
21.9
< 0.1
25.2
5.9
16
11.7
14.3
24.4
13.1
9.7
0.001
44.8
368
1.9
9.6
7.3
< 0.1
9.3
7.3
18.9
12.1
3.2
3.6
15.8
12.7
0.001
> 200
95
2.4
51.5
316
0.9
6.8
514
1270
477
28.3
9.7
336
338
0.04
> 200
543
4.8
78.8
27.9
3.3
160
15.5
36.6
19.4
16.9
27
180
185
0.022
156
977
2
79.3
33
0.6
175
45
98
54.7
36.9
43.4
150
161
0.019
64
278
1.8
69.7
37.4
0.6
102
16.6
38.3
20.5
20.6
30.9
Makkovik
Makkovik
49,628
49,628
50,111
50,111
Postville
Postville
50,109
50,109 50,601
50,601
50,405
50,405 50,501
50,501
50,101
50,112
50,112 50,113
50,113
50,101
50,403
50,403
50,408
50,408
50,502
50,502
50,114
50,114
50,503
50,503
50,402
50,402
50,404
50,404 50,407
50,407
50,102
50,102
50,602
50,602
50,110
50,110
0
2.5
5
kilometers
50,406
50,406
50,504
50,504
50,509
50,509
50,508
50,508
50,108
50,108
50,106
50,106
50,507
50,507
50,510
50,510
50,105
50,105
50,506
50,506
50,505
50,505 50,103
50,103
50,001
50,001
50,104
50,104
50,107
50,107
50,007
50,007
50,702
50,702
50,202
50,202
50,701
50,701
50,120
50,120
49,902
49,902
50,801
50,801
50,201
50,201
49,905
49,905
49,904
49,904
Bayswater/UCore
J.V. Claims
15
15
00
50,302
50,302
30
30
kilometers
kilometers
Sample_#
U
ppm
UDNC
U308
Th
ppm
%
ppm
0.1
TD-MS
0.1
DNC
0.001
DNC
Zr
Zn
ppm
Nb
ppm
La
ppm
Ce
ppm
Nd
ppm
ppm
0.1
1
0.2
0.1
0.1
0.1
0.1
TD-MS
TD-MS
TD-MS
TD-MS
TD-MS
TD-MS
TD-MS
49628
63.2
63.1
0.007
16.1
172
28.1
11.5
47.6
90
30.3
49902
626
674
0.079
> 200
> 5000
482
> 500
41.8
214
231
49904
195
205
0.024
51.3
244
29.8
36.1
47.7
127
67.7
49905
32.4
33.8
0.004
83.1
379
19.1
103
35.9
70.5
32.5
50001
48.6
51.7
0.006
43.8
549
16.3
28.4
10.3
26.9
10.4
50007
297
314
0.037
> 200
2110
308
181
98.5
226
122
50101
9.5
9.6
0.001
10
21
13.7
8.3
1.2
3.6
3
50102
60.9
66.2
0.008
> 200
257
72.7
60.5
24.2
54.5
31.7
50103
100
100
0.012
161
174
55
63.5
3.3
12.6
18.3
50104
169
173
0.02
> 200
1270
244
284
34.4
142
123
50105
54.2
53.2
0.006
141
45
48.9
102
2
10.4
18.8
50106
61.4
64.8
0.008
123
82
38.9
57.6
1.5
7
11.5
50107
78.5
90
0.011
> 200
434
38
57.9
1.9
8.7
14.8
50108
26.2
28.5
0.003
46.4
69
21.8
21.3
7.1
17.3
10.2
50109
252
247
0.029
> 200
473
169
4.9
55.3
174
204
50110
388
381
0.045
> 200
2090
82
102
6.5
32.1
39.3
50111
142
153
0.018
> 200
737
25.8
58
3.5
16
29.9
50112
148
144
0.017
> 200
366
31.9
9.1
1.6
10.8
24.8
50113
23.4
17.6
0.002
51.6
22
12.3
30.5
0.5
2.2
4.2
50114
4.7
3.6
< 0.001
51.5
391
74.9
10
56.8
127
53.6
50120
191
194
0.023
175
343
174
87.7
44.8
109
50.1
50201
222
247
0.029
> 200
1600
131
117
25.6
98.5
72.2
50202
168
189
0.022
> 200
2200
74.9
> 500
5.1
26.8
24.7
50302
513
533
0.063
50.6
850
110
52.9
109
175
80.2
50402
75.2
59.9
0.007
66.7
151
23.1
10
1.1
4.1
7
50403
160
143
0.017
> 200
484
68.2
15.9
4.1
15.8
24.6
50404
56.5
44.3
0.005
93.5
43
41.4
11.3
3.1
10.6
10.7
50405
62.3
34
0.004
102
40
22.7
45.5
2
7.3
9.9
50406
64.8
49.5
0.006
76.2
456
30.7
46
1.1
4.7
6.5
50407
22.5
20
0.002
14.7
8
14.6
43.4
2.2
7.1
7.4
50408
62.9
46.7
0.006
106
26
8.6
14.3
0.9
5.6
12.9
50501
34.9
27.9
0.003
69.4
36
52.5
8.2
14.5
41.3
25.2
50502
33.9
25.1
0.003
60
6
31.3
14.4
0.8
2.8
3.6
50503
54.4
62.8
0.007
157
75
10.9
11.6
14.2
32.2
16.7
50504
105
88.9
0.01
144
405
28.4
27.8
8
21.4
16.5
50505
149
165
0.02
> 200
190
409
90.9
20.6
77.2
99.7
50506
148
163
0.019
> 200
318
89.5
42.4
21.1
81.1
83.5
50507
124
103
0.012
191
108
37.4
36.4
14.9
36.8
26.5
50508
80.2
63.7
0.008
98.8
211
69.9
181
1.4
6
6.8
50509
61.9
50.5
0.006
80.1
403
25.7
70
2.4
6.3
7.4
50510
116
96.2
0.011
128
682
21.9
25.2
5.9
16
11.7
50601
13.1
9.7
0.001
44.8
368
7.3
9.3
7.3
18.9
12.1
50602
15.8
12.7
0.001
> 200
95
316
6.8
514
1270
477
50701
336
338
0.04
> 200
543
27.9
160
15.5
36.6
19.4
50702
180
185
0.022
156
977
33
175
45
98
54.7
50801
150
161
0.019
64
278
37.4
102
16.6
38.3
20.5
0
2.5
5
kilometers
Bayswater/UCore J.V. Claims
Central Mineral Belt, Labrador
Makkovik River Project
2008 Sample Location Map
Scale 1:40,000
NTS 13J/11,12,14
Produced by: DF
NAD27, Zone 20
November 2008
APPENDIX C
Activation Laboratories Assay Sheets
Final Report
Activation Laboratories
Report: A08-4304 rev 1 Rev, 1
Report Date: 8/19/2008
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
49621
49622
49623
49624
49625
49626
49719
50201
50202
Au
ppb
5
TD-MS
30
33
29
39
33
<5
8
64
448
Li
ppm
0.5
TD-MS
8.2
9.7
3.2
2.9
2.7
8.2
32.3
4.9
5
Na
%
0.001
TD-MS
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
2.48
2.79
> 3.00
Mg
%
0.01
TD-MS
1.69
1.09
0.36
0.38
0.46
0.89
2.27
0.02
0.01
Al
%
0.01
TD-MS
7
3.41
9.18
8.09
9.25
7.99
8.9
5.88
5.85
K
%
0.01
TD-MS
0.77
0.71
0.04
0.05
0.06
0.11
1.93
2.13
0.82
Ca
%
0.01
TD-MS
5.06
3.44
0.47
1.04
1.49
7.48
3.26
0.17
0.13
Cd
ppm
0.1
TD-MS
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.5
0.1
0.1
V
ppm
1
TD-MS
63
45
10
28
31
95
190
4
10
Cr
ppm
0.5
TD-MS
24.3
20.5
9.7
13.3
19.3
45.8
189
18.7
12.8
Mn
ppm
1
TD-MS
758
544
134
266
306
525
724
371
153
Page 1 of 3
Fe
%
0.01
TD-MS
3.38
2.25
1.58
4.43
4.45
4.4
5.85
2.55
3.55
Hf
ppm
0.1
TD-MS
6.5
4.6
6.5
7.6
8
0.3
2.7
40.4
60.9
Ni
ppm
0.5
TD-MS
14
11.3
2
2.4
2.8
3.6
104
1.3
1.3
Er
ppm
0.1
TD-MS
2.5
1.2
2.3
3.8
5.9
40.8
1.8
88.4
64.7
Be
ppm
0.1
TD-MS
6.4
5.6
2.1
2
2.2
4.9
3.8
3.5
6.3
Ho
ppm
0.1
TD-MS
0.9
0.5
0.5
1
1.7
13.2
0.6
25.4
17.5
Ag
ppm
0.05
TD-MS
0.08
0.08
0.09
0.13
0.06
0.07
0.51
< 0.05
< 0.05
Cs
ppm
0.05
TD-MS
0.7
0.73
0.29
0.12
0.15
0.16
12.6
0.53
0.35
Co
ppm
0.1
TD-MS
12.4
9.3
1.4
3
2.7
2.5
27.6
1
1.3
Eu
ppm
0.05
TD-MS
2.2
1.17
0.29
0.65
0.83
7.67
0.98
1.77
0.96
Final Report
Report Date: 8/19
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
49621
49622
49623
49624
49625
49626
49719
50201
50202
Bi
ppm
0.02
TD-MS
< 0.02
< 0.02
< 0.02
0.32
0.11
< 0.02
0.07
< 0.02
< 0.02
Se
ppm
0.1
TD-MS
0.5
0.3
0.2
0.4
0.6
4.2
1.5
6.9
4.8
Zn
ppm
0.2
TD-MS
83.9
61.6
12.2
22
25.2
19
144
131
74.9
Ga
ppm
0.1
TD-MS
29.1
20.7
24.2
22.8
25.5
19.7
18.1
26.4
32.8
As
ppm
0.1
TD-MS
0.5
1.2
< 0.1
1.4
2.5
19.1
< 0.1
2.8
1.8
Rb
ppm
0.2
TD-MS
11.4
5.7
1.4
1
1
6.9
152
146
73.5
Y
ppm
0.1
TD-MS
18.4
7.4
14.9
27.9
46.2
359
16
585
416
Sr
ppm
0.2
TD-MS
516
394
30.7
46.6
63.8
294
208
30.4
21.3
Zr
ppm
1
TD-MS
310
201
260
298
300
34
165
1600
2200
Nb
ppm
0.1
TD-MS
15.7
15.9
13.3
17.3
16.8
1.3
6.2
117
> 500
Mo
ppm
0.1
TD-MS
0.6
0.6
0.4
38.6
3
0.8
106
1.8
0.6
Page 2 of 3
In
ppm
0.1
TD-MS
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
Sn
ppm
1
TD-MS
2
2
3
3
3
<1
5
6
11
Sb
ppm
0.1
TD-MS
0.7
0.5
0.2
0.3
0.4
< 0.1
0.4
< 0.1
0.3
Te
ppm
0.1
TD-MS
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
Ba
ppm
1
TD-MS
709
766
22
76
60
149
669
108
27
La
ppm
0.1
TD-MS
59.6
30.7
4.3
19.9
27.1
238
22.2
25.6
5.1
Ce
ppm
0.1
TD-MS
119
69.5
10.2
42
59.8
648
39.2
98.5
26.8
Pr
ppm
0.1
TD-MS
16.3
9.1
1.4
5.5
8
93.9
5.3
16.1
4.6
Nd
ppm
0.1
TD-MS
47.8
27.9
5
18
25.7
324
17.2
72.2
24.7
Sm
ppm
0.1
TD-MS
7.2
4
1
3.1
4.4
56.2
2.9
26.6
13.8
Final Report
Report Date: 8/19
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
49621
49622
49623
49624
49625
49626
49719
50201
50202
Gd
ppm
0.1
TD-MS
5.8
3.2
1.1
3.3
4.8
54
3.1
48.5
28.5
Tb
ppm
0.1
TD-MS
0.9
0.4
0.2
0.5
0.8
8.4
0.4
10.8
7.1
Dy
ppm
0.1
TD-MS
5
2.5
1.4
3.6
6.2
55.2
2.8
89.4
60.7
Cu
ppm
0.2
TD-MS
3.8
2.9
3.6
4.3
4.3
2.6
165
2.8
1.9
Ge
ppm
0.1
TD-MS
0.3
0.4
< 0.1
0.2
0.3
0.9
0.2
0.3
0.2
Tm
ppm
0.1
TD-MS
0.3
0.2
0.5
0.7
1.1
6
0.2
13.4
10.7
Yb
ppm
0.1
TD-MS
1
< 0.1
5.2
7.5
9.3
42.8
0.9
104
90.5
Lu
ppm
0.1
TD-MS
< 0.1
< 0.1
0.9
1.4
1.5
5.7
< 0.1
15.9
15
Ta
ppm
0.1
TD-MS
0.8
0.8
1
1.1
1.5
< 0.1
0.3
3
14.8
W
Re
ppm
ppm
0.1
0.001
TD-MS TD-MS
0.3
0.002
0.5
0.003
< 0.1
0.003
0.6
0.004
0.4
0.003
< 0.1 < 0.001
0.7
0.876
< 0.1
0.001
12.2
0.002
Page 3 of 3
Tl
ppm
0.05
TD-MS
0.18
0.22
< 0.05
< 0.05
< 0.05
< 0.05
1.21
0.71
0.3
Pb
ppm
0.5
TD-MS
509
324
24.1
18.7
27.5
64.9
301
171
153
Th
ppm
0.1
TD-MS
7.4
3.5
24.2
18.3
28.9
> 200
18.5
> 200
> 200
U
U
ppm ppm
0.1
0.1
TD-MS DNC
890
969
351
513
169
182
45.8
62
68.2 81.4
283
303
891
965
222
247
168
189
U3O8
%
0.001
DNC
0.114
0.061
0.021
0.007
0.01
0.036
0.114
0.029
0.022
Mass
g
DNC
1.024
1.086
1.043
1.01
1.073
1.038
1.026
1.074
1.091
Au
ppb
5
FA-AA
11
Final Report
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
49627
49628
49901
49902
49903
49904
49905
50001
50101
50102
50103
50104
50105
50106
50107
50108
50109
50110
50111
50112
50113
50114
50301
50302
50401
50402
50403
50404
50405
50406
50407
50408
50501
50502
50503
50504
50505
50506
50507
50508
50509
50510
50601
50602
Au
ppb
5
TD-MS
<5
9
7
428
7
21
59
37
5
22
25
114
21
21
14
17
24
216
121
28
20
25
14
106
13
20
32
<5
18
29
12
<5
6
<5
<5
42
52
22
7
125
41
47
20
12
Li
ppm
0.5
TD-MS
15.6
16.1
16.2
2.7
14
1.9
11.5
2
11.3
9.1
3.3
3.6
3.7
5.2
1.5
3.4
0.7
3.1
7.9
5.2
1.6
13.6
29.1
8.8
16.7
3.9
4.1
7.4
8.1
2.3
3.5
1.3
3
6.5
4.8
1.3
0.5
0.5
2.2
2.3
0.6
0.5
< 0.5
43.8
Na
%
0.001
TD-MS
> 3.00
> 3.00
> 3.00
1.57
2.53
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
1.53
> 3.00
> 3.00
> 3.00
2.99
2.14
1.98
> 3.00
> 3.00
> 3.00
> 3.00
2.9
> 3.00
2.09
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
2.88
> 3.00
1.96
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
> 3.00
1.95
Mg
%
0.01
TD-MS
2.4
0.06
0.55
0.02
0.46
0.04
0.38
0.01
0.02
0.01
0.01
0.02
0.01
0.02
< 0.01
0.01
0.01
0.08
0.01
< 0.01
< 0.01
0.38
1.94
0.06
0.97
0.01
0.01
0.01
0.01
< 0.01
0.01
< 0.01
0.01
0.01
0.01
0.01
0.01
0.01
0.02
0.01
0.01
< 0.01
0.01
3.37
Al
%
0.01
TD-MS
9.27
7.02
> 10.0
1.96
6.99
6.92
9.62
7.53
8.21
6.24
7.59
3.42
6.2
6.64
7.51
6.22
3.22
3.48
5.78
6.09
6.37
6.77
7.55
6.54
5.31
6.08
4.61
5.9
7.46
5.75
5.68
6.41
6.4
6.82
3.74
5.03
2.74
4.95
6.02
4.56
5.4
5.38
7.39
3.74
K
%
0.01
TD-MS
1.02
1.36
1.62
0.5
0.92
0.08
2.07
0.9
3.97
1.05
0.5
1.32
0.97
1.01
0.61
2.07
1.45
1.73
3.06
1.97
2.33
4.2
0.98
0.11
0.65
4.04
2.18
3.43
2.06
0.4
3.24
3.9
1.96
4.36
1.16
2.22
0.89
1.73
3.09
2.24
2.79
1.73
2.16
0.45
Ca
%
0.01
TD-MS
5.16
0.04
2.64
0.31
1.82
0.33
2.85
0.07
0.11
0.15
0.1
0.16
0.17
0.04
0.06
0.08
0.15
0.13
0.43
0.12
0.16
1.26
2.91
0.94
2.19
0.07
0.28
0.22
0.23
0.17
0.19
0.05
0.05
0.17
0.18
0.05
0.07
0.08
0.14
0.1
0.04
0.05
0.18
17.3
Cd
ppm
0.1
TD-MS
< 0.1
< 0.1
< 0.1
0.9
< 0.1
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.3
< 0.1
< 0.1
0.1
< 0.1
0.2
0.4
0.1
0.1
< 0.1
0.1
0.1
0.3
0.1
< 0.1
0.1
< 0.1
< 0.1
0.2
< 0.1
< 0.1
0.1
< 0.1
< 0.1
0.1
0.1
0.1
< 0.1
0.2
0.1
0.1
0.1
0.3
V
ppm
1
TD-MS
74
10
39
4
31
46
30
2
1
2
1
68
2
2
1
1
2
5
1
1
<1
16
71
235
6
1
1
1
1
1
1
1
1
1
<1
1
<1
1
1
<1
1
<1
1
474
Cr
ppm
0.5
TD-MS
52.6
9.1
35.7
14.6
14.8
6.8
128
6.4
8.1
8.8
10.5
33
11.1
8.6
14.3
6.2
16
13.9
7.7
6.8
5.9
9
31
5.8
14.6
9.4
10.6
6.7
7.6
8.7
4.2
8
6.4
6.2
4.4
13
16.2
11.2
6.1
23.1
7.6
9
6.2
32.2
Mn
ppm
1
TD-MS
937
468
266
1100
207
365
308
67
71
440
277
857
194
164
208
109
434
302
233
169
86
517
885
673
758
126
241
142
156
185
97
59
210
96
97
168
1230
319
127
180
93
132
68
1810
Page 1 of 3
Fe
%
0.01
TD-MS
4.76
0.97
2.36
11.7
1.65
2.57
3.94
0.94
0.75
4.68
1.18
11.6
1.49
1.24
2.15
0.83
5.03
3.42
0.86
0.93
0.69
2.44
5.3
4.09
5.46
0.84
2.84
1.16
1.35
1.03
0.64
0.86
0.96
0.85
0.85
1.81
11.8
3.95
1.17
0.89
0.76
1.76
0.94
3.31
Hf
ppm
0.1
TD-MS
1.6
5.7
4.4
154
6.8
5
13.6
26.1
0.9
8.4
6.7
41.1
1.6
2.6
9.8
2.7
13.3
84
30.8
11.5
0.7
9.8
2.4
23.8
4.6
4.8
13.3
1.1
3
14.8
0.3
1.1
1.8
0.2
2.6
13.5
6.3
8
3.4
7.6
12
22.2
10.9
2.1
Ni
ppm
0.5
TD-MS
54.1
1.1
8.2
1.2
11.8
1.6
1.2
1.1
1.2
1.1
1.3
2.1
1.6
2.2
1
1
1.2
1.5
0.9
0.9
1
2.4
23.8
1.9
3.2
1.3
1.1
0.9
1.2
1.1
1.1
0.9
0.7
0.8
0.7
1
0.9
0.8
0.9
0.8
0.9
0.8
0.9
47.6
Er
ppm
0.1
TD-MS
1.8
2.3
0.6
259
1.7
11.3
16.7
7.8
1.9
29
34.6
152
34.1
22.2
30.5
7
55
85.9
82.7
56.3
11.7
6.7
2.8
14.5
7.7
16.3
47.4
8.7
14.4
17.4
14.8
36.3
15.2
6.8
12
25.7
152
106
18.4
11.2
11.9
17.7
3
14.8
Be
ppm
0.1
TD-MS
3.2
1.6
2.3
1.2
1.1
2.8
0.9
2
1.4
2.3
1.4
5.2
0.9
0.9
2.2
2
4.4
2.6
3.5
2.6
2.1
2.6
1
13.8
0.9
2.1
1.7
2.2
2.1
3
2.2
2.8
3.6
2
2.4
1.8
1.3
2.3
2.5
1.8
1.7
1.8
4.6
8.9
Ho
ppm
0.1
TD-MS
0.8
0.7
0.2
76.6
0.6
4
5.1
1.6
0.6
8.8
9.9
43.9
10.3
6.3
8.9
2
19.6
22.8
24
16.9
3.5
2.2
1
4.6
2.7
4.7
14.7
2.9
4.3
5
4.3
10.8
4.1
2.2
3.7
6.7
44.5
31.1
5.7
3.1
3.2
4.6
0.9
6.1
Ag
ppm
0.05
TD-MS
< 0.05
0.07
0.05
< 0.05
< 0.05
0.18
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
0.29
0.53
< 0.05
0.1
< 0.05
0.09
0.16
0.18
0.29
0.08
0.1
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
0.06
< 0.05
< 0.05
< 0.05
< 0.05
< 0.05
0.08
0.15
0.12
Cs
ppm
0.05
TD-MS
1.68
2.22
3.26
0.55
1.39
0.49
0.71
0.87
1.67
1.5
1.19
0.92
1.07
2.22
0.46
1.05
0.24
0.18
0.82
0.36
0.27
0.77
1.21
0.27
0.57
0.82
0.51
0.8
0.71
0.24
0.56
0.38
0.56
0.76
0.39
0.46
0.2
0.28
0.71
0.55
0.36
0.29
0.35
0.71
Co
ppm
0.1
TD-MS
22.5
0.3
6
3
6.4
2.5
1.6
0.6
0.4
0.6
0.4
4.4
0.8
0.6
0.4
0.4
0.9
1.3
0.3
0.4
0.2
3.6
14.8
2.2
30.1
0.4
0.5
0.4
0.4
0.4
0.3
0.3
0.3
0.3
0.4
0.3
0.7
0.4
0.4
0.2
0.4
0.2
0.4
22.5
Eu
ppm
0.05
TD-MS
2.49
0.27
0.98
5.9
0.45
0.8
0.63
0.1
0.15
0.52
0.38
2.36
0.53
0.27
0.37
0.2
2.96
0.95
0.76
0.55
0.14
1.15
1.11
0.62
2
0.26
0.71
0.4
0.29
0.16
0.21
0.43
0.22
0.19
0.27
0.31
2.2
1.87
0.43
0.15
0.17
0.18
0.22
8.2
Final Report
Report Date: 08/1
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
49627
49628
49901
49902
49903
49904
49905
50001
50101
50102
50103
50104
50105
50106
50107
50108
50109
50110
50111
50112
50113
50114
50301
50302
50401
50402
50403
50404
50405
50406
50407
50408
50501
50502
50503
50504
50505
50506
50507
50508
50509
50510
50601
50602
Bi
ppm
0.02
TD-MS
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
0.03
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
< 0.02
1.47
Se
ppm
0.1
TD-MS
< 0.1
< 0.1
< 0.1
23.2
< 0.1
1.3
1.2
< 0.1
< 0.1
2.1
2.3
13.1
2.5
1.9
2.7
< 0.1
6.2
5.6
6.3
4.3
0.8
0.7
0.9
1.8
2.3
1.1
3.6
0.6
1.5
1.3
0.9
2.3
0.9
0.5
0.7
1.3
11.1
7.7
1.1
0.7
0.7
1
0.3
2.3
Zn
ppm
0.2
TD-MS
94
28.1
54.9
482
37.8
29.8
19.1
16.3
13.7
72.7
55
244
48.9
38.9
38
21.8
169
82
25.8
31.9
12.3
74.9
82
110
52.8
23.1
68.2
41.4
22.7
30.7
14.6
8.6
52.5
31.3
10.9
28.4
409
89.5
37.4
69.9
25.7
21.9
7.3
316
Ga
ppm
0.1
TD-MS
23
22.6
29.2
22.3
19.8
27.3
31
50.2
33.1
35.8
44.2
31.2
32.9
37.6
54.2
31.7
23.9
22.4
43.3
35.6
35.7
22.8
19.6
53.2
24.7
34.1
30.3
32.6
33.8
37.7
29.3
35.3
42.4
34.6
22.2
35.3
33.2
41
38.2
41.9
40.8
37.7
40.7
19.9
As
ppm
0.1
TD-MS
0.8
< 0.1
< 0.1
7.5
< 0.1
5.9
1.1
< 0.1
< 0.1
< 0.1
< 0.1
3.4
< 0.1
< 0.1
< 0.1
< 0.1
2.9
1.3
2.3
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
2.2
1.8
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
419
Rb
ppm
0.2
TD-MS
41.1
68
42.3
28.6
45.6
2.5
97.3
86.3
218
75.9
25.7
85
71.7
72.2
37.3
126
72.9
83.7
268
155
167
146
38.4
2.9
28.3
283
155
231
145
34.1
210
267
144
268
88
145
70.3
105
204
183
195
121
125
26.6
Y
ppm
0.1
TD-MS
16
19
6.2
1430
13.3
94.1
118
54
18.4
170
250
895
212
144
195
42.1
301
382
434
266
81.5
55.8
24.5
122
63.9
98.7
226
66.4
95.3
109
88.4
188
110
41.7
75.7
155
742
531
106
79.9
78.6
110
22.3
162
Sr
ppm
0.2
TD-MS
776
2.4
765
59
129
67.7
706
12.1
8.6
14.8
4.3
50.3
3.9
4.2
4.4
8.3
14.6
25.7
6.2
5.4
5.7
205
150
21.4
179
5
4.8
7.2
6.2
2.9
11.4
6.1
6.8
6.4
5.2
9.5
3.9
11.8
7.6
3.5
4
3.8
22.9
477
Zr
ppm
1
TD-MS
109
172
206
> 5000
227
244
379
549
21
257
174
1270
45
82
434
69
473
2090
737
366
22
391
103
850
163
151
484
43
40
456
8
26
36
6
75
405
190
318
108
211
403
682
368
95
Nb
ppm
0.1
TD-MS
0.3
11.5
5.1
> 500
13.2
36.1
103
28.4
8.3
60.5
63.5
284
102
57.6
57.9
21.3
4.9
102
58
9.1
30.5
10
0.7
52.9
2.6
10
15.9
11.3
45.5
46
43.4
14.3
8.2
14.4
11.6
27.8
90.9
42.4
36.4
181
70
25.2
9.3
6.8
Mo
ppm
0.1
TD-MS
0.3
1.3
0.3
1
15.9
1.3
0.4
0.2
0.4
0.9
0.4
0.9
0.3
0.4
0.6
0.5
0.3
0.3
0.4
< 0.1
< 0.1
2.6
< 0.1
0.1
0.7
0.3
0.2
0.1
0.2
0.3
0.1
< 0.1
0.9
0.3
0.1
0.3
< 0.1
0.8
0.4
0.2
0.3
< 0.1
< 0.1
0.9
Page 2 of 3
In
ppm
0.1
TD-MS
< 0.1
< 0.1
< 0.1
0.1
< 0.1
0.2
0.1
< 0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
0.1
0.4
0.2
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
< 0.1
< 0.1
0.1
0.2
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
Sn
ppm
1
TD-MS
<1
2
2
16
1
4
5
3
1
3
1
16
1
1
3
1
1
3
2
1
<1
1
<1
13
1
1
2
1
1
1
1
<1
1
1
<1
1
1
2
1
1
1
1
1
1
Sb
ppm
0.1
TD-MS
0.1
< 0.1
< 0.1
0.4
< 0.1
0.3
0.1
0.3
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.2
0.2
0.1
< 0.1
< 0.1
0.1
< 0.1
0.4
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
4.5
Te
ppm
0.1
TD-MS
< 0.1
< 0.1
< 0.1
0.4
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.2
0.1
< 0.1
< 0.1
< 0.1
0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
Ba
ppm
1
TD-MS
892
13
1430
65
489
100
232
35
80
65
13
225
11
12
7
57
72
61
26
9
14
886
343
26
223
29
20
47
17
5
90
26
31
54
18
62
11
29
61
13
11
7
87
167
La
ppm
0.1
TD-MS
97.1
47.6
34.7
41.8
24.7
47.7
35.9
10.3
1.2
24.2
3.3
34.4
2
1.5
1.9
7.1
55.3
6.5
3.5
1.6
0.5
56.8
12.8
109
12.4
1.1
4.1
3.1
2
1.1
2.2
0.9
14.5
0.8
14.2
8
20.6
21.1
14.9
1.4
2.4
5.9
7.3
514
Ce
ppm
0.1
TD-MS
196
90
63.7
214
52.6
127
70.5
26.9
3.6
54.5
12.6
142
10.4
7
8.7
17.3
174
32.1
16
10.8
2.2
127
29.2
175
30.3
4.1
15.8
10.6
7.3
4.7
7.1
5.6
41.3
2.8
32.2
21.4
77.2
81.1
36.8
6
6.3
16
18.9
1270
Pr
ppm
0.1
TD-MS
22.3
9.8
6.5
39.2
5.4
17.7
8.7
3
0.6
7.4
2.9
23.4
2.7
1.7
2.2
2.3
40.1
6.3
4.2
3.1
0.6
14.9
3.9
24.9
4.6
1
3.6
2
1.6
1
1.4
1.7
6.3
0.5
4.4
3.4
17
15.8
5.7
1.1
1.4
2.5
2.8
144
Nd
ppm
0.1
TD-MS
74.9
30.3
20.5
231
17.9
67.7
32.5
10.4
3
31.7
18.3
123
18.8
11.5
14.8
10.2
204
39.3
29.9
24.8
4.2
53.6
15.7
80.2
20.7
7
24.6
10.7
9.9
6.5
7.4
12.9
25.2
3.6
16.7
16.5
99.7
83.5
26.5
6.8
7.4
11.7
12.1
477
Sm
ppm
0.1
TD-MS
10.6
4.5
2.8
> 100
3.3
17.1
9.5
2.6
1.2
11.8
10.7
56.9
12.5
7
9.1
3.4
74.1
21.2
20.6
18.6
3
10.6
3.6
15.3
6.5
4.7
16.3
4.7
5.4
4.9
3.9
9.3
8.1
2.3
5.5
6.8
51.3
37.8
9.2
3.6
3.7
5
2.8
65.5
Final Report
Report Date: 08/1
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
49627
49628
49901
49902
49903
49904
49905
50001
50101
50102
50103
50104
50105
50106
50107
50108
50109
50110
50111
50112
50113
50114
50301
50302
50401
50402
50403
50404
50405
50406
50407
50408
50501
50502
50503
50504
50505
50506
50507
50508
50509
50510
50601
50602
Gd
ppm
0.1
TD-MS
6.7
3.2
1.9
178
2.9
16.3
12.3
2.8
1.8
19.2
18.6
91.6
21.9
11.9
16.3
4.6
90.6
36.7
40.5
36.2
6.3
10.7
4.1
16.3
9.3
9.3
31.4
7.6
9.7
9.9
7.5
19.9
9.8
4.5
8.2
11.7
94.1
63.9
13.3
6
6
8.2
3.1
56.8
Tb
ppm
0.1
TD-MS
0.8
0.5
0.2
38.8
0.4
3.1
2.8
0.7
0.3
4.3
4.4
20.8
5.1
2.8
3.8
1
16.2
9.7
10.9
8.5
1.6
1.8
0.7
3
1.8
2.4
7.3
1.6
2.2
2.4
2.1
5.1
2.1
1.1
1.9
2.9
22.2
15.1
3.1
1.5
1.5
2.1
0.6
6.5
Dy
ppm
0.1
TD-MS
3.7
2.9
1.2
283
2.5
19.1
20.4
5.3
2.3
32.8
34.4
157
37.8
22.3
30.3
7.3
81
70
74.3
55.8
11.3
9.1
3.8
17.1
10.5
16.3
47.8
9.6
14.9
16
14.3
34.7
13.4
7.4
12.3
20
147
101
19.3
10
10
14.3
3.2
28.3
Cu
ppm
0.2
TD-MS
11.2
3.8
2.4
4.3
7.7
22.7
1.4
4
46.5
4.7
4.9
13.4
2.8
9.7
1.5
5.2
4.3
87.7
3.9
5.4
2
5.8
91.2
5.3
288
4.2
3.2
2.6
1.4
2.7
1.9
1.9
2.6
2.2
1.6
7.7
3.2
2.5
3.6
2
2.6
2.2
1.9
2.4
Ge
ppm
0.1
TD-MS
0.3
0.2
0.4
1.4
0.3
0.2
0.6
0.1
0.3
0.7
< 0.1
0.4
0.8
0.1
< 0.1
< 0.1
1.3
0.5
0.4
0.2
0.1
1
0.2
1.3
0.6
0.2
0.2
0.2
0.4
0.1
0.1
0.2
0.2
0.2
0.2
0.5
0.6
0.8
0.8
0.7
0.2
0.2
0.2
1.3
Tm
ppm
0.1
TD-MS
0.3
0.4
0.1
42
0.2
1.7
2.8
1.9
0.3
4.2
5.8
23.7
5.2
3.7
5
1.2
7.8
16.4
13.1
8.7
1.8
1
0.4
2.3
1.2
2.6
6.9
1.2
2.2
2.7
2.3
5.7
2.8
1
1.9
4.7
23.4
16.7
2.8
1.9
2.1
3.3
0.5
1.8
Yb
ppm
0.1
TD-MS
0.4
2.9
< 0.1
> 200
1.1
10.6
19
18.3
1.8
25.9
37.4
144
30.6
24.1
33.1
8.6
44.2
126
90.8
54.2
10.7
6.1
2.6
16.9
7.4
16
41.7
7.6
13.3
18
14.1
34.1
21.4
5.8
11.9
36.1
140
99.5
17
13.3
16.3
24.4
3.6
9.7
Lu
ppm
0.1
TD-MS
< 0.1
0.5
< 0.1
39.6
< 0.1
1.4
2.9
3.9
0.2
3.6
5.4
19.9
3.9
3.4
4.8
1.2
6.1
22.1
14.1
8.7
1.5
0.8
0.4
3
1.1
2.5
6.4
1.1
2
3
2
4.8
3.7
0.8
1.9
6.8
18.1
14.5
2.5
2.1
2.9
4.5
0.6
1.3
Ta
ppm
0.1
TD-MS
< 0.1
0.6
0.2
29.5
0.2
1
4.5
2.4
0.1
1.3
1.6
7.3
1.2
1.2
1.1
0.6
0.1
3
1.5
0.1
0.4
0.3
< 0.1
2.3
< 0.1
0.1
0.2
< 0.1
0.5
0.4
0.6
0.1
0.1
0.1
< 0.1
0.6
1.4
0.1
0.1
4
0.8
0.4
0.1
0.3
W
ppm
0.1
TD-MS
< 0.1
< 0.1
0.1
9.8
< 0.1
0.5
1.2
0.1
< 0.1
0.2
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
Re
ppm
0.001
TD-MS
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
< 0.001
0.002
0.002
< 0.001
< 0.001
0.003
0.002
0.008
0.004
0.002
< 0.001
0.002
< 0.001
< 0.001
0.004
< 0.001
< 0.001
0.001
< 0.001
< 0.001
< 0.001
< 0.001
0.001
0.001
0.001
0.002
< 0.001
0.002
Page 3 of 3
Tl
ppm
0.05
TD-MS
0.31
0.51
0.35
0.16
0.33
< 0.05
0.8
0.68
1.42
0.87
0.12
0.5
0.54
0.43
0.18
0.88
0.34
0.39
1.2
0.69
0.67
0.87
0.2
< 0.05
0.17
1.31
0.69
1.1
0.75
0.15
0.98
1.13
0.6
1.27
0.42
0.64
0.3
0.45
0.94
0.88
0.92
0.54
0.49
0.11
Pb
ppm
0.5
TD-MS
99.6
43.5
30
230
59.8
161
13.1
21.8
14.4
107
59.6
98.8
18.2
25.8
28.4
16.6
82.3
104
39.6
98.9
16.3
28
8.5
177
5.5
30
98.3
48.5
29.6
20.6
19
26.6
56.4
27.2
36.4
40
58.6
56.7
53
33.1
28.9
42.3
9.6
51.5
Th
ppm
0.1
TD-MS
11.1
16.1
8.4
> 200
128
51.3
83.1
43.8
10
> 200
161
> 200
141
123
> 200
46.4
> 200
> 200
> 200
> 200
51.6
51.5
9
50.6
6
66.7
> 200
93.5
102
76.2
14.7
106
69.4
60
157
144
> 200
> 200
191
98.8
80.1
128
44.8
> 200
U
U U3O8
ppm ppm
%
0.1
0.1 0.001
TD-MS DNC
DNC
339
337
0.04
63.2 63.1 0.007
17.3 17.4 0.002
626
674 0.079
63 65.5 0.008
195
205 0.024
32.4 33.8 0.004
48.6 51.7 0.006
9.5
9.6 0.001
60.9 66.2 0.008
100
100 0.012
169
173
0.02
54.2 53.2 0.006
61.4 64.8 0.008
78.5
90 0.011
26.2 28.5 0.003
252
247 0.029
388
381 0.045
142
153 0.018
148
144 0.017
23.4 17.6 0.002
4.7
3.6 < 0.001
2.3
1.8 < 0.001
513
533 0.063
5.8
3 < 0.001
75.2 59.9 0.007
160
143 0.017
56.5 44.3 0.005
62.3
34 0.004
64.8 49.5 0.006
22.5
20 0.002
62.9 46.7 0.006
34.9 27.9 0.003
33.9 25.1 0.003
54.4 62.8 0.007
105 88.9
0.01
149
165
0.02
148
163 0.019
124
103 0.012
80.2 63.7 0.008
61.9 50.5 0.006
116 96.2 0.011
13.1
9.7 0.001
15.8 12.7 0.001
Mass
g
DNC
1.053
1.067
1.008
1.031
1.064
1.062
1.011
1.038
1.054
1.058
1.07
1.041
1.063
1.078
1.072
1.01
1.069
1.045
1.044
1.038
1.068
1.038
1.09
1.065
1.052
1.056
1.053
1.083
1.05
1.047
1.047
1.03
1.059
1.009
1.075
1.015
1.092
1.058
1.059
1.03
1.059
1.073
1.005
1.078
Au
ppb
5
FA-AA
<5
<5
Final Report
Report: A08‐5998
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
50121
50122
50123
50124
50125
50126
50701
50702
50703
50704
50705
50706
50707
50708
50709
50710
50801
50802
50803
50804
50805
50806
49720
49721
49722
49723
49724
50007
50008
50009
50010
50011
50012
50013
50014
50015
50016
50017
50018
50019
50020
50021
50022
50023
50024
50025
50026
Au
ppb
5
TD-MS
87
34
41
11
43
78
75
206
227
48
48
38
57
79
53
48
51
225
87
59
76
59
77
55
51
41
66
20
298
11
70
7
5
45
17
52
65
52
38
45
54
108
47
40
26
64
51
163
Li
ppm
0.5
TD-MS
4.1
3.5
5.9
10.7
11.8
2.9
3.1
3
0.8
11.9
15.1
3.1
3.7
10
10.1
3.2
25
5.1
7.1
6.7
1.7
7.9
8.1
11.3
6
2.5
7.3
7.4
1.4
12.2
15.8
48.7
10.7
10.8
8.5
11
17.7
46.5
4.4
10.9
2.2
2.6
4
7.6
2.2
4.7
5
6.3
Na
%
0.001
TD-MS
> 3.00
0.433
2.31
0.284
> 3.00
0.345
0.309
1.86
> 3.00
1.37
1.43
2.17
0.222
> 3.00
0.154
1.56
0.054
2.7
> 3.00
0.396
2.05
> 3.00
> 3.00
1.5
0.338
0.323
0.266
0.526
2.46
2.54
0.198
2.02
0.845
1.42
1.05
0.83
1.75
0.081
0.205
0.077
2.98
0.441
> 3.00
0.441
2.64
> 3.00
> 3.00
> 3.00
Mg
%
0.01
TD-MS
0.01
0.17
0.29
0.4
0.64
0.21
0.1
0.04
0.01
0.32
0.4
0.11
0.28
0.51
0.71
0.22
2.05
0.02
0.13
0.4
0.07
0.44
0.28
0.53
0.36
0.12
0.6
0.55
0.01
0.69
0.43
1.55
1.19
1.06
0.67
0.78
0.6
3.32
0.4
0.38
0.1
0.11
0.32
0.46
0.14
0.11
0.24
0.26
Al
%
0.01
TD-MS
6.12
6.45
9.56
9.68
8.98
6.08
4.92
4.91
6.27
6.44
5.42
7.08
5.01
9.22
8.47
8.54
4.66
6.12
> 10.0
7.51
5.89
9.04
8.91
6.03
7.14
5.58
5.24
9.26
4.87
7.2
2.66
7.91
6.49
7.36
6.14
8.77
8.92
9.33
4.4
5.88
8.75
7.21
8.89
9.52
8.76
8.8
> 10.0
> 10.0
K
%
0.01
TD-MS
1.16
2.14
3.29
3.53
2.99
2.33
3.43
1.37
1.03
1.28
1.66
2.12
2.79
0.8
3.85
2.18
1.62
1.21
3.14
> 5.00
1.8
1.6
0.89
0.83
3.24
2.54
3.2
4.18
1.08
2.11
1.28
1.09
0.71
1.14
0.63
1.11
1.3
1.35
1.21
0.81
2.61
1.97
3.18
4.16
4.12
1.91
0.73
1.09
Ca
%
0.01
TD-MS
0.13
0.32
0.6
0.08
0.32
0.31
0.61
0.15
0.16
0.47
0.69
0.47
0.49
0.51
0.58
0.14
0.11
0.14
0.12
0.16
0.06
0.11
0.43
1.38
0.74
0.5
0.08
0.16
0.09
2.68
5.41
1.15
2.85
6.2
3.51
10.2
8.68
9.28
5.56
2.01
0.31
0.14
0.68
0.1
0.18
0.25
0.32
0.22
Cd
ppm
0.1
TD-MS
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
0.1
0.1
0.1
0.1
< 0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
1.2
0.2
0.8
0.2
0.3
0.5
0.4
0.8
0.7
1
0.6
0.3
< 0.1
< 0.1
0.1
0.1
0.1
< 0.1
< 0.1
< 0.1
V
ppm
1
TD-MS
2
74
42
22
61
55
160
4
3
28
32
122
123
62
104
55
63
5
56
44
79
32
45
27
57
65
84
58
2
29
86
140
41
64
42
93
61
98
31
37
74
24
89
42
44
57
16
29
Cr
ppm
0.5
TD-MS
10.7
14.3
8.2
20.4
9.3
13.2
11
10.1
12.4
32.2
43
5
14.8
10.7
9
5.6
227
19.4
12.2
9.4
8.3
5
5.6
28.5
8.5
9.9
11.6
5.4
9
66.2
44.2
112
40.3
34.9
28.8
29
24.8
40.1
31.7
29.6
6
18.8
6.3
9.4
8.2
5
4.8
5.4
Page 1 of 8
Mn
ppm
1
TD-MS
727
245
494
305
648
209
451
171
142
288
203
329
366
872
724
175
1390
118
110
513
129
364
251
386
586
291
805
518
616
917
931
387
604
860
554
1200
959
2400
643
286
288
240
561
482
158
166
278
318
Fe
%
0.01
TD-MS
2.14
11.2
2.3
3.13
5.99
8.31
23.3
1.85
2.05
1.32
1.11
11.2
18.7
6.41
4.6
5.72
6.57
1.57
8.34
7.22
11.3
2.62
1.68
1.4
9.89
8.41
15.7
2.96
2.96
2.93
4.48
6.56
2.6
3.35
1.93
4.22
3.76
8.15
1.93
1.72
6.7
2.94
6.91
3.42
3.18
9.18
2.71
1.65
Hf
ppm
0.1
TD-MS
10.8
5.8
5.1
5.7
6.7
4
4.5
15.9
31.6
1.8
14.8
3.2
3.3
8.1
4.9
5.1
3.5
10.5
8.2
4.7
9.5
5.6
5.2
0.1
5
4.3
7.4
5.7
68.4
4
14.2
1.9
0.3
5.7
0.7
5.5
6
7.1
6
2.9
3.5
5.5
4
5
4.5
6.6
5.6
4.6
Ni
ppm
0.5
TD-MS
3.3
3.7
2.5
3.7
2.4
3.1
2.6
1.3
0.9
8.5
8.1
1.5
1.5
2
5.1
1.2
57.1
0.9
0.7
2.9
1.3
1.6
3
8.1
2.8
4.3
4.9
2.7
0.8
5.6
21.6
87.7
20.5
23.5
18.4
25.1
21.3
72.2
10.4
12.4
1.4
1.2
2.9
4.2
3.9
0.5
1
1.3
Er
ppm
0.1
TD-MS
50.5
9.5
6.6
8.4
17.6
21.8
69.9
19.3
36.7
3.1
2.2
16.5
41.8
9
45.9
12.2
6.2
24.3
8.4
6.1
7.5
7.4
7.1
2.6
17.9
16.2
87.1
16.9
94.2
2.3
4.6
1.4
3.4
4.6
3.8
5.8
5.5
8
3
2.8
5.6
18
6.3
9.4
9.8
15.6
10.8
6.7
Be
ppm
0.1
TD-MS
3.6
1.4
1.1
2
1.3
1.9
1.6
2.8
3.4
1.8
1.8
0.5
0.8
3.9
1.2
1.6
1.3
4.8
7.8
2.4
4.3
2.6
2.5
1.9
1.3
1.7
1.4
1.4
2.5
1.6
2.7
0.6
2
2.3
1.9
2.9
3
3.3
1.4
2.2
0.7
0.7
1
0.8
1
9.5
7
2
Ho
ppm
0.1
TD-MS
13.5
2.9
2.1
2.7
5.2
6.8
19.2
5.2
10.5
1
0.8
5
11.6
3
12.9
3.7
1.9
6.4
2.7
2
2.3
2.3
2.3
0.9
5.1
5
24.3
4.8
26
0.8
1.6
0.5
1.2
1.6
1.3
2
1.9
3
1.2
1
1.8
5.3
2.1
2.8
3
5.1
3.4
2.2
Ag
ppm
0.05
TD-MS
< 0.05
7.52
0.58
0.09
11.1
27.8
22.1
< 0.05
< 0.05
0.12
0.2
0.31
22.5
0.31
18.2
18.4
12.4
< 0.05
0.05
0.15
1.61
0.17
> 100
0.45
1.55
8.98
16.9
11.5
0.39
0.12
0.3
0.11
< 0.05
0.06
0.07
0.1
0.37
0.71
5.58
0.14
0.41
34.4
1.15
7
0.29
< 0.05
18.6
> 100
Cs
ppm
0.05
TD-MS
0.62
1.64
2.52
3.84
5.4
1.19
1.14
0.75
1.02
2.02
2.04
1.13
1.12
4.79
3.22
1.46
14.1
1.15
1.44
4.09
1.26
2.86
2.85
1.89
3.26
1.51
6.26
2.37
0.84
2.85
1.34
2.23
1.86
1.34
1.48
1.55
1.49
1.63
2.23
3.65
1.35
1.8
1.66
4.13
1.22
1.5
1.77
2.35
Co
ppm
0.1
TD-MS
3.9
2.2
3.9
2.8
2.6
15.3
21.9
0.7
0.9
4
4.2
1.6
2.5
3.3
46.8
2.8
14.3
0.7
0.6
3.7
1.1
1.9
6.1
4.7
3.4
36.8
8.1
13.8
1.5
5.4
9.7
25.7
10.8
13.8
8.7
13.4
8
49.1
7.5
4.1
0.8
1.4
2.8
13.6
4
0.5
1.8
3
Final Report
Report: A08‐5998
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
49654
Au
ppb
5
TD-MS
87
18
Li
ppm
0.5
TD-MS
4.1
101
Na
%
0.001
TD-MS
> 3.00
2.08
Mg
%
0.01
TD-MS
0.01
1.79
Al
%
0.01
TD-MS
6.12
3.17
K
%
0.01
TD-MS
1.16
1.4
Ca
%
0.01
TD-MS
0.13
3.99
Cd
ppm
0.1
TD-MS
0.1
0.1
V
ppm
1
TD-MS
2
195
Cr
ppm
0.5
TD-MS
10.7
60.8
Page 2 of 8
Mn
ppm
1
TD-MS
727
1340
Fe
%
0.01
TD-MS
2.14
7.72
Hf
ppm
0.1
TD-MS
10.8
< 0.1
Ni
ppm
0.5
TD-MS
3.3
37.2
Er
ppm
0.1
TD-MS
50.5
3
Be
ppm
0.1
TD-MS
3.6
2.7
Ho
ppm
0.1
TD-MS
13.5
1.2
Ag
ppm
0.05
TD-MS
< 0.05
0.87
Cs
ppm
0.05
TD-MS
0.62
6.71
Co
ppm
0.1
TD-MS
3.9
35.1
Final Report
Report: A08‐5998
Report Date: 10/
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
50121
50122
50123
50124
50125
50126
50701
50702
50703
50704
50705
50706
50707
50708
50709
50710
50801
50802
50803
50804
50805
50806
49720
49721
49722
49723
49724
50007
50008
50009
50010
50011
50012
50013
50014
50015
50016
50017
50018
50019
50020
50021
50022
50023
50024
50025
50026
Eu
ppm
0.05
TD-MS
0.88
1.58
1.18
1.41
2.66
2.69
6.64
0.34
1.03
0.92
0.76
1.62
3.49
2.33
4.98
2.23
1.32
0.47
1.14
1.31
0.97
1.26
1.17
0.91
1.76
2.67
6.72
1.83
2.42
1.7
1.52
0.82
1.15
1.5
1.13
1.75
2.04
3.99
1.49
1.02
0.93
1.86
1.24
1.56
0.98
1.8
1.04
1.4
Bi
ppm
0.02
TD-MS
< 0.02
0.76
0.05
< 0.02
0.14
1.65
2.06
0.14
< 0.02
0.22
0.39
0.07
0.53
< 0.02
2.22
1.7
4.13
< 0.02
< 0.02
< 0.02
0.1
< 0.02
3.23
0.77
1.57
1.7
13.7
2.55
1
0.54
0.95
0.23
0.12
0.2
< 0.02
0.05
0.14
0.63
0.62
0.07
< 0.02
8.65
1.3
1.29
0.3
0.21
0.23
0.38
Se
ppm
0.1
TD-MS
4.6
6.8
4.9
1.5
2.7
5.5
10.3
1.8
3.3
0.5
0.8
7.1
4.3
1.2
12
2.5
1.4
2
1
0.8
1.3
1
13
0.9
2.5
6.3
14.8
3.1
7.8
0.6
0.7
0.6
0.7
0.7
0.5
0.7
0.8
1.7
0.8
0.4
0.7
4.7
6.2
2.2
1.1
1.9
1.4
2.6
Zn
ppm
0.2
TD-MS
174
14.6
19.6
35.4
35.1
10.5
32.1
27.9
33
34.8
26.8
20.8
22.3
43.7
21.7
14.1
99
37.4
8.4
44.9
10.8
44.9
18.8
38.2
36.6
10.3
64.1
23.7
308
99.4
36.6
94.7
48.4
53.1
32.7
37.9
28.2
146
27.1
25
17.6
13.9
37.4
29.5
12.5
8.2
25.2
21.2
Ga
ppm
0.1
TD-MS
32.3
12.9
12.3
16.5
26.8
9.9
10.4
28.5
38.9
15.7
14.4
13.2
9.2
31.2
20.8
16
34.5
33.2
27.7
22.7
12.3
22.9
35
14.4
19.4
11.4
33.8
20.3
32.2
15.3
26.8
19.7
16
19.6
14.4
25.8
23.1
31.7
8.3
13.9
12.4
7.5
15.4
19.4
11.7
27.7
29.6
30.6
As
ppm
0.1
TD-MS
1.5
5.6
1.9
10.5
7.9
92.3
17.1
4.1
2.4
8.9
11.6
3
119
13.6
29.4
50.2
5.4
3.7
22.4
2.7
17
36
9.4
8
3.1
6.4
7.7
32
6.1
2.6
5.4
19
0.9
0.3
< 0.1
3.1
4.4
0.3
45.3
4.5
1.6
6.8
3
1.3
3.9
6.9
4.1
4.9
Rb
ppm
0.2
TD-MS
114
101
100
141
143
83.8
109
110
103
61.7
79.7
65.9
95.5
82.8
111
84.6
149
106
133
210
101
125
76.8
47.8
135
91
157
137
105
86.7
25
54.2
41.3
52.9
36.5
51.2
59.7
50.5
55.2
53.4
83.1
86.5
89.9
165
124
83.9
56.4
58.1
Y
ppm
0.1
TD-MS
287
75.3
55.7
73.2
127
164
464
115
221
26.4
19.9
104
259
76.1
338
97.3
52.2
153
63.1
52.1
47.5
55.7
56.4
23.4
126
126
558
122
540
21.8
32.9
12.6
31.5
43.9
35.7
54.1
53
71
33.8
24.8
43.7
111
53.5
72.9
77.7
121
88.8
56.7
Sr
ppm
0.2
TD-MS
12.6
35.5
81.6
39.7
89.9
32.8
52.4
28.6
16.9
29.8
35.7
44.2
31
66.2
79.5
45.8
2.7
29.9
55
37.5
22.8
52.7
93.3
49.4
37.1
34.1
26.3
49.2
15.9
282
440
61.5
171
356
178
513
485
613
85.2
30.3
58.2
30.5
63.9
43.9
48.8
59.3
54.7
51.8
Zr
ppm
1
TD-MS
343
196
170
180
216
140
151
543
977
100
532
105
114
296
167
170
138
278
287
171
292
198
174
14
159
156
239
184
2110
194
625
83
23
249
47
281
327
424
369
111
119
168
152
165
148
247
184
143
Page 3 of 8
Nb
ppm
0.1
TD-MS
87.7
13.9
16.9
1.7
16.7
11.5
41.3
160
175
8.6
14.1
18.6
35.8
34.4
25.9
15.6
8
102
26.8
26.5
26.5
29.2
25.3
6.7
24.9
14.1
55.3
9
181
3.1
25.7
1.2
2.3
11.9
4.6
12.1
11.1
13.7
9.3
8.6
18.5
17.1
17.7
15.7
9.9
24.3
6.5
9.1
Mo
ppm
0.1
TD-MS
0.6
1.7
1.1
0.2
0.9
1.7
1
3.3
0.6
3.5
6.5
0.7
1.3
3.2
11.7
11.8
53.3
0.6
1.3
0.9
2.9
2.7
6310
128
48.3
11.5
156
19.3
5.2
< 0.1
6.1
1.6
1.1
1
0.8
0.5
0.5
0.6
11.8
1.6
1
35.2
4.5
8.4
3
2.3
4.7
38.8
In
ppm
0.1
TD-MS
0.1
0.1
0.1
0.1
0.2
0.1
0.2
< 0.1
< 0.1
< 0.1
< 0.1
< 0.1
0.1
0.1
0.2
0.1
0.1
< 0.1
0.1
0.1
0.1
0.1
0.1
< 0.1
0.1
0.2
0.1
0.1
0.1
< 0.1
0.1
0.1
0.1
0.1
< 0.1
0.1
0.1
0.1
< 0.1
0.1
< 0.1
< 0.1
< 0.1
0.1
< 0.1
0.1
0.1
0.1
Sn
ppm
1
TD-MS
3
8
4
1
7
7
22
5
7
2
4
4
19
9
10
8
1
4
7
4
10
6
3
1
4
12
6
7
8
1
6
<1
1
3
1
4
3
4
2
3
4
4
3
4
3
7
3
2
Sb
ppm
0.1
TD-MS
0.1
0.5
0.4
0.1
0.4
1
1.6
0.1
0.1
2.9
4.9
0.5
2.5
0.5
3.3
0.8
0.3
< 0.1
0.6
0.3
1
0.7
0.4
2.4
0.7
0.7
1.5
1
0.1
0.3
3.3
< 0.1
0.2
0.9
0.4
1.4
2.1
2.6
11.5
2
0.4
0.4
0.5
0.3
0.2
0.4
0.2
0.5
Te
ppm
0.1
TD-MS
0.2
6.8
0.4
< 0.1
5.3
10.1
12.9
0.1
0.1
< 0.1
0.1
0.3
12.5
0.2
14
9.5
13.7
0.1
0.1
0.2
1.7
0.2
71.3
8
3.9
7.3
14.8
7.9
1
0.1
0.7
0.3
0.3
0.2
0.2
< 0.1
0.1
0.1
0.1
< 0.1
0.8
30.2
2.8
5.3
0.4
0.2
7.9
175
Ba
ppm
1
TD-MS
46
727
821
684
622
689
614
228
61
395
357
543
606
191
966
688
182
115
516
767
619
551
93
367
825
697
592
967
41
1040
409
454
337
305
301
373
352
383
1260
352
665
712
687
831
735
439
77
173
La
ppm
0.1
TD-MS
44.8
131
122
113
158
137
160
15.5
45
36.9
27.8
41.9
96.1
127
186
212
36.8
16.6
51.3
101
51.2
74.9
63.7
33.3
71.6
178
39
67.6
98.5
59.6
20.9
16.1
53.5
61.9
50.1
57.2
45.4
45.5
28.5
31.4
56.3
50
67.9
107
48.4
77.1
82.5
46
Ce
ppm
0.1
TD-MS
109
235
221
197
287
250
299
36.6
98
71.5
63
81.6
180
224
346
424
73.2
38.3
96
176
107
142
121
67.9
130
337
88.5
138
226
100
45.7
28.4
90.7
92.1
78.6
97.1
80.4
93
56.3
68.4
96.1
104
116
184
87.8
138
152
88.1
Pr
ppm
0.1
TD-MS
13.5
33.4
31.5
28.6
40.3
36.6
43.5
5.1
14.6
8.8
6.9
13.2
26.4
31.7
49.3
55.9
9.7
5.4
13.4
24.8
15.9
18.6
16
8.3
18.7
48.4
14.9
20.6
32.9
13.9
6.4
4
12.8
15
11.7
14
11.2
13.8
7.2
7.7
13.9
14.9
16.9
26
11.9
19.9
20.5
11.6
Final Report
Report: A08‐5998
Report Date: 10/
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
49654
Eu
ppm
0.05
TD-MS
0.88
3.67
Bi
ppm
0.02
TD-MS
< 0.02
0.07
Se
ppm
0.1
TD-MS
4.6
0.9
Zn
ppm
0.2
TD-MS
174
166
Ga
ppm
0.1
TD-MS
32.3
24.9
As
ppm
0.1
TD-MS
1.5
< 0.1
Rb
ppm
0.2
TD-MS
114
103
Y
ppm
0.1
TD-MS
287
16
Sr
ppm
0.2
TD-MS
12.6
977
Zr
ppm
1
TD-MS
343
32
Page 4 of 8
Nb
ppm
0.1
TD-MS
87.7
0.1
Mo
ppm
0.1
TD-MS
0.6
0.4
In
ppm
0.1
TD-MS
0.1
0.1
Sn
ppm
1
TD-MS
3
1
Sb
ppm
0.1
TD-MS
0.1
0.1
Te
ppm
0.1
TD-MS
0.2
< 0.1
Ba
ppm
1
TD-MS
46
1670
La
ppm
0.1
TD-MS
44.8
60.4
Ce
ppm
0.1
TD-MS
109
120
Pr
ppm
0.1
TD-MS
13.5
19.1
Final Report
Report: A08‐5998
Report Date: 10/
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
50121
50122
50123
50124
50125
50126
50701
50702
50703
50704
50705
50706
50707
50708
50709
50710
50801
50802
50803
50804
50805
50806
49720
49721
49722
49723
49724
50007
50008
50009
50010
50011
50012
50013
50014
50015
50016
50017
50018
50019
50020
50021
50022
50023
50024
50025
50026
Nd
ppm
0.1
TD-MS
50.1
109
99.5
92.4
128
125
157
19.4
54.7
28.7
23
45.7
90.9
104
173
174
31.1
20.5
44.1
79.7
51.9
58.3
50.6
27.3
61.8
163
71.1
71.5
122
44.2
21.9
13.4
39.7
48.8
37.7
46.8
38.2
52.4
25.3
25.4
43.2
53
54.5
82.2
39.5
67.6
63
38.1
Sm
ppm
0.1
TD-MS
15.8
17.7
14.5
15.6
22.5
26.8
41.9
6.2
16
5.2
4.2
11.3
23.4
19.2
34.7
26.1
6.2
6.9
9.4
13.3
9.7
10.9
10.4
5.1
13.9
29.3
38.8
16.1
37.1
6.4
5.1
2.6
6.2
8.6
6.2
8.8
8
13.7
5.7
4.9
7.9
15.6
10.1
13.7
7.9
15
11.3
8.5
Gd
ppm
0.1
TD-MS
25.6
13.5
11.3
13.5
21.7
26.2
53.3
9.6
24.3
5.1
4.1
13.3
29.1
18.1
38.9
20
6.5
11.5
10.2
10.9
8.7
10
9.7
5
15.7
24.6
58.3
16
57
5.3
6
2.6
5.8
8
6.2
9.3
8.8
15
6.8
5.2
7.5
17.5
9.8
12.2
8.8
17.3
12.8
9
Tb
ppm
0.1
TD-MS
5.9
1.9
1.5
2
3.2
4.5
9.8
2.2
4.9
0.7
0.6
2.7
5.6
2.4
7
2.5
1.1
2.7
1.8
1.5
1.5
1.5
1.6
0.7
2.8
3.5
12.1
2.6
12
0.6
1.1
0.4
0.8
1.2
0.9
1.5
1.4
2.5
1
0.8
1.2
3.1
1.5
1.8
1.6
3.1
2.1
1.6
Dy
ppm
0.1
TD-MS
44.3
11.7
8.8
11.6
19.9
27.8
69.1
16.9
36.9
4.4
3.3
18.9
40.2
13.4
47.6
14.7
7.4
20.6
11.1
8.3
9.5
9
9.7
4
18.6
20.9
85.6
17.2
87.6
3.4
6.7
2.1
4.7
7
5.5
8.7
8.2
14.4
5.3
4.2
7.1
20
8.5
10.6
11.2
20.3
13.2
9.7
Cu
ppm
0.2
TD-MS
4.1
14.3
142
2.1
23.2
99.1
183
4.8
2
60.8
103
53.5
9
41.6
347
11.9
1.7
1.8
0.6
3.3
4.7
7.9
31.1
53.1
27
52.2
60
31.2
1.7
2.4
89.2
99.3
21.1
18.9
21.2
41.3
77.7
225
990
40
4.1
90.7
105
233
26.2
0.9
71.5
40
Ge
ppm
0.1
TD-MS
0.2
0.4
0.3
0.3
1.1
0.9
0.8
0.2
0.2
0.7
0.1
0.3
0.8
0.7
0.9
1.2
0.5
0.2
0.5
0.7
0.3
0.3
0.4
0.2
0.8
0.8
0.8
0.8
0.6
0.3
0.4
0.2
0.4
1.4
0.3
2
1.5
2.7
0.2
0.1
0.2
0.3
0.3
0.5
0.4
0.5
0.6
0.6
Tm
ppm
0.1
TD-MS
9.5
1.6
1.1
1.3
3.1
3.8
12.9
3.7
6.6
0.5
0.4
2.9
7.6
1.5
8.5
2
1
4.5
1.5
1
1.2
1.3
1.2
0.4
3.3
2.7
16.7
3.1
17
0.4
0.7
0.2
0.5
0.7
0.6
0.9
0.9
1.1
0.4
0.4
0.9
3.2
1.1
1.6
1.7
2.6
1.7
1.1
Yb
ppm
0.1
TD-MS
62.5
11
7.1
8
21.5
25
94.9
27
43.4
2.8
2
20
57.3
10.2
59.7
14.1
6.9
30.9
9.8
6.7
7.4
8
8.5
2.2
23.1
18
124
21.7
115
1.8
4
1.3
3.1
4.2
3.4
5.3
4.9
6.2
1.8
2.6
6.1
22.5
6.7
10.6
10.9
16.4
11.7
7.6
Lu
ppm
0.1
TD-MS
9.8
1.6
0.9
1.1
3.4
3.4
14.1
4.7
6.9
0.4
0.2
2.7
8.5
1.5
9.7
2.1
1.1
5.1
1.4
0.9
1
1
1.3
0.3
3.4
2.5
18.3
3.4
19.1
0.1
0.5
0.1
0.4
0.6
0.5
0.7
0.7
0.7
< 0.1
0.3
0.8
3.2
0.9
1.6
1.6
2.4
1.9
1.1
Page 5 of 8
Ta
ppm
0.1
TD-MS
1.8
0.2
0.8
< 0.1
0.3
0.3
0.5
3.6
4.1
0.4
0.7
0.5
0.3
1.3
0.4
0.4
0.3
4.7
1.4
1
1
1
0.3
0.2
0.9
0.2
0.6
< 0.1
3.8
< 0.1
1
< 0.1
0.1
0.8
0.3
0.9
0.8
0.7
0.5
0.5
0.9
0.5
0.7
0.6
0.3
1.1
0.1
0.1
W
ppm
0.1
TD-MS
< 0.1
12.3
1.2
< 0.1
2.2
2.3
49.8
3.3
7.4
1.7
4
0.3
18.7
2
3
2.2
0.7
2.7
12.7
2.1
14
1.8
2.7
1.2
14.9
4.4
34.3
0.8
0.5
0.1
3
0.1
< 0.1
0.1
< 0.1
< 0.1
0.4
0.8
5.1
1.6
0.1
0.5
0.3
1.7
0.1
18.5
2.1
0.9
Re
ppm
0.001
TD-MS
< 0.001
0.001
0.006
0.002
< 0.001
0.002
0.01
0.011
< 0.001
0.004
0.002
0.006
0.008
0.002
0.011
0.002
0.012
< 0.001
0.001
0.002
0.005
0.005
0.791
0.004
0.006
0.002
0.034
0.005
0.017
0.001
0.004
0.007
0.004
0.003
0.003
< 0.001
0.003
0.004
0.005
0.001
0.003
0.002
0.001
0.005
0.003
0.004
0.006
0.009
Tl
ppm
0.05
TD-MS
0.97
1.11
1
1.78
1.43
0.96
0.79
0.96
0.63
0.69
0.81
0.61
0.81
0.93
1.31
1.19
2.14
1.11
0.65
1.74
1.05
0.98
0.69
0.61
1.49
0.99
1.69
1.35
0.86
0.66
0.51
0.4
0.5
0.37
0.43
0.51
0.43
0.36
0.52
0.71
0.73
1.29
0.77
1.81
0.86
0.51
0.29
0.33
Pb
ppm
0.5
TD-MS
102
667
298
145
654
1600
4540
78.8
79.3
31
47
766
2050
342
3030
794
918
69.7
198
224
264
188
457
46.4
663
1360
3320
557
121
61
635
8.3
61.7
128
126
198
516
1010
1980
94.1
314
759
342
559
412
195
117
676
Th
ppm
0.1
TD-MS
175
32.1
37
33.8
47.6
23.6
28.8
> 200
156
28
40
17.2
21.8
41
27.8
27.6
26.3
64
51.8
28.3
21.9
35.7
31.5
11.8
24.4
23.1
36.2
33.3
> 200
10
15.4
4.7
13.2
21.6
10.8
24.2
20.8
20.3
15.2
14.9
18
23.5
22.5
28.1
28.4
33.9
43.5
19.8
U
ppm
0.1
TD-MS
191
3570
1380
644
3870
9470
> 10000
336
180
161
160
4130
> 10000
1460
> 10000
5190
5210
150
800
1140
1380
833
1360
132
3830
6840
> 10000
3810
297
355
536
9
114
210
173
271
690
749
6220
247
1380
3390
1420
2570
2290
1050
481
2540
U
ppm
0.1
DNC
194
3630
1350
644
4000
8800
> 10000
338
185
157
166
4710
> 10000
1430
> 10000
5250
5590
161
789
1170
1400
917
1400
126
4160
7200
> 10000
3960
314
367
703
7.5
112
225
186
272
704
783
6660
253
1420
3650
1490
2770
2470
1100
471
2730
U3O8
%
0.001
DNC
0.023
0.428
0.16
0.076
0.471
1.04
> 1.18
0.04
0.022
0.018
0.02
0.555
> 1.18
0.169
> 1.18
0.619
0.659
0.019
0.093
0.139
0.166
0.108
0.166
0.015
0.491
0.849
> 1.18
0.467
0.037
0.043
0.083
0.001
0.013
0.027
0.022
0.032
0.083
0.092
0.786
0.03
0.168
0.43
0.176
0.327
0.291
0.129
0.056
0.322
Mass
g
DNC
1.062
1.05
1.067
1.04
1.076
1.028
1.043
1.025
1.065
1.049
1.083
1.052
1.077
1.078
1.09
1.052
1.07
1.047
1.05
1.022
1.032
1.038
1.057
1.085
1.08
1.053
1.062
1.093
1.028
1.022
1.041
1.033
1.043
1.063
1.064
1.056
1.078
1.014
1.027
1.03
1.052
1.041
1.088
1.041
1.032
1.041
1.065
1.016
U3O8
%
0.005
FUS-XRF
3.48
1.75
2.66
2.56
Final Report
Report: A08‐5998
Report Date: 10/
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
49654
Nd
ppm
0.1
TD-MS
50.1
71.4
Sm
ppm
0.1
TD-MS
15.8
12.9
Gd
ppm
0.1
TD-MS
25.6
10.1
Tb
ppm
0.1
TD-MS
5.9
1.3
Dy
ppm
0.1
TD-MS
44.3
5.7
Cu
ppm
0.2
TD-MS
4.1
33.1
Ge
ppm
0.1
TD-MS
0.2
0.7
Tm
ppm
0.1
TD-MS
9.5
0.3
Yb
ppm
0.1
TD-MS
62.5
1.2
Lu
ppm
0.1
TD-MS
9.8
< 0.1
Page 6 of 8
Ta
ppm
0.1
TD-MS
1.8
0.2
W
ppm
0.1
TD-MS
< 0.1
< 0.1
Re
ppm
0.001
TD-MS
< 0.001
0.004
Tl
ppm
0.05
TD-MS
0.97
0.49
Pb
ppm
0.5
TD-MS
102
26.4
Th
ppm
0.1
TD-MS
175
1.8
U
ppm
0.1
TD-MS
191
15.7
U
ppm
0.1
DNC
194
11.3
U3O8
%
0.001
DNC
0.023
0.001
Mass
g
DNC
1.062
1.018
U3O8
%
0.005
FUS-XRF
Report: A08‐5998
Report Date: 10/
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
50121
50122
50123
50124
50125
50126
50701
50702
50703
50704
50705
50706
50707
50708
50709
50710
50801
50802
50803
50804
50805
50806
49720
49721
49722
49723
49724
50007
50008
50009
50010
50011
50012
50013
50014
50015
50016
50017
50018
50019
50020
50021
50022
50023
50024
50025
50026
Final Report
Au
ppb
5
FA-AA
<5
<5
<5
<5
Page 7 of 8
Report: A08‐5998
Report Date: 10/
Analyte Symbol
Unit Symbol
Detection Limit
Analysis Method
50120
49654
Final Report
Au
ppb
5
FA-AA
Page 8 of 8
APPENDIX D
Bayswater/UCore 2008 Claims Map
Makkovik
Makkovik
012818M
012818M
012819M
012819M
Postville
Postville
012798M
012798M
012795M
012795M
012820M
012820M
012787M
012787M
0
2.5
012825M
012825M
5
kilometers
012790M
012790M
012794M
012794M
012793M
012793M
012832M
012832M
Bayswater/UCore
J.V. Claims
012796M
012796M
012830M
012830M
00
15
15
30
30
kilometers
kilometers
012831M
012831M
012784M
012784M
012786M
012786M
012788M
012788M
012777M
012777M
012791M
012791M
012822M
012822M
012821M
012821M
012803M
012803M
012780M
012780M
012801M
012801M
012775M
012775M
012829M
012829M
012808M
012808M
012747M
012747M
012735M
012735M
012809M
012809M
0
2.5
5
kilometers
012768M
012768M
Bayswater/UCore J.V. Claims
Central Mineral Belt, Labrador
Makkovik River Project
Claims Location Map
Scale 1:40,000
NTS 13J/11,12,14
Produced by: DF
NAD27, Zone 20
November 2008

bayswater uranium corporation - Government of Newfoundland and

Transcription

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