Pernambuco-Paraíba Basin

PERNAMBUCO & PARAÍBA
BASINS
Geol. Mário de Lima Filho, DSc
Assessoria DIR I
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Location
Área Total – 33,000 Km2
Terra – 9,000 Km2
Mar – 24,000 Km2
SPEPB-AP2
North Limit
Mamanguape High
Natal Plattform
PB
North Limit
Pernambuco Lineament
Paraíba Basin
PE
SPEPB-AP3
South Limit
Maragogi High
Alagoas Basin
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Infraestructure and
Operacionais Conditions
BR-222-CE – To Pecém Port
Transnordestina
Railway
101 Hwy
Suape Port
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Exploratory Datas
• Gravimetric Coverage
• Magnetometry Coverage
• Seismic: 10,078 km
• Seismic Spec: 960 km
• Wells (land): 3 (the most deep
with 3.000m, others with
1,100m and 400m)
• Surface Mapping (FunpecUFRN)
• Surface Geochemistry and
piston core survey
• Evaluation Study on Potential
Petroleum Pernambuco-Paraiba
Basins - ANP/Funpec/UFRN
CURRENT STAGE OF
BLOCKS ROUND 9
Seismic 3D Acquisition
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Tectono-Stratigraphy
Evolution
In the early Aptian rifting Pernambuco Basin
Matos,1999
Reconstruction Drift Phase (postTuronian) beginning of Rift Paraíba
Basin
Tectono-Stratigraphy
Evolution
Regional
Context
Continental Crust x Oceanic
Crust Limit
3 Structural Domains (A,B and C)
Fonte: ANP/FUNPEC
Differences between
PE&PB Basins
Lagese, 2004
Oliveira, 1995
Differences between
PE&PB Basins
Barbosa et al, 2004
Stratigraphic
Chart
Post-Rift
Rift
Paraíba Basin
Barbosa,2007
Paraíba Basin
48-RL-592
Regional
Context
Piedade Graben
Cupe Graben
Maracatu High
Alagoas Basin
Lamont-Doherty in the Oceanic Domain
Datas
Pernambuco Basin
Bouguer Residual Anomaly
-Maracatu High
-1,2 e 3 Vulcanics
Rocks
Almeida et al,2005
Pernambuco Basin
-Basement Structural Map
- Tectonic Aspect
- 6,000 m Depocenters
Structural
Framework
Sistema de
Falhas do
Frevo
Legenda
Discordância Mioceno
Alto do
Maracatu
Charneira do
embasamento
coincidente com
falha expressiva
Discordância K-T
Discordância Rifte-Drifte
Embasamento
Charneira do Embasamento
Reflexões
intra-embasamento
Line 250-RL-370
5 km
Structural
Framework
27-RL-568/103-RL-256 Composite Line
2-CPE-1-PE
2-CPE-01-PE
NW
Graben do Cupe
SE
Alto do Maracatu
103-RL-256
27-RL568
3 km
SUB-BACIA DE PERNAMBUCO
Linha Composta 27-RL-568 / 103-RL-256
Legenda
Discordância Mioceno
Discordância K-T
Discordância Rifte-Drifte
Embasamento
Pernambuco Plateau
Bouguer
Residual Map
Recife
Seismic
Structural Map
Filtro passa-banda
10-50 Km
Halocinetic Structures
Halocinetic Structures
Line 250-371
Salt
Halocinetic Structures
250-RL-378
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Petroleum
Systems
• Geochemical Study
-Land – Surface Survey
Anomalies Identifications of the gaseous HC
- Sea - Piston core Survey
- Anomalies identification of heavy gaseous HC.
Indications of processes of generation and migration hydrocarbons
Geochemical
Survey
34°0'0"W
33°0' 0"W
6°0'0"S
7°0'0"S
8°0'0"S
9°0'0"S
9°0'0"S
8°0'0"S
7°0'0"S
6°0'0"S
5°0'0"S
35°0'0"W
5°0'0"S
36°0'0"W
36°0'0"W
35°0'0"W
34°0'0"W
33°0' 0"W
Contour map of ratio
(C1+C2+C3)/(C4+C5) on the basis of
the well sediments, this ratio directly
reflects the tendency of occurring light
hydrocarbons
Geochemical
Survey
35°0'0 "W
34°0'0 "W
33°0'0 "W
4°0'0"S
33°0'0 "W
6°0'0"S
7°0'0"S
8°0'0"S
9°0'0"S
9°0'0"S
8°0'0"S
7°0'0"S
6°0'0"S
5°0'0"S
34°0'0 "W
5°0'0"S
4°0'0"S
Distribution of oil exudation of Map
35°0'0 "W
Geochemical
Survey
Almost all samples exhibit
composition originated from
sources generating oil
Speculative
Volumes
Project Evaluation ANP / FUNPEC / UFRN:
Potential sub-basin of Pernambuco in situ volumes: 2 billion bbl,
considering only economically accumulations.
Possibles
Reservoirs
Turbidites Deposits of the Calumbi
Formation/Terciary age (same in SergipeAlagoas basins).
Fluvial sandstones of the Algodoais
Formation- Paleogen age.
Carbonates of the Estiva
Formation/Cenomanian-Turonian
age.
Fluvials sandstones, fan-delta and deltas of the
Cabo Formation/ Rift phase, and turbidites
sandstones in facies of the botton lake.
Possibles
Reservoirs
Carbonates of the Gramame and Maria
Farinha formations - Maastrichtian e Terciáry
age.
Clastics Sediments of the
Beberibe and Itamaracá
formations - upper
Cretaceous age.
Events Chart
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Plays
Expectative
Play type 1 - Associated with
topographically elevated region of
Maracatu High;
Play type 2 – Mixing of the Cabo
Formation with stratigraphic traps
and mixing, associated presence
of the evaporites. Reservoir and
generator of the Cabo Formation;
Plays
Expectative
Play type 3 – Post-Rift with traps mix and
paleogeomorphic in turbidites.
Play type 4 – Associated to the vulcanic
rocks inside with sedimentary rocks in the
Plateau region.
Jiyang Basin
Changzhi Wu et al, 2006
Zalán et al, 1985
Plays
Expectative
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Analogous Exploratory
Successes
Brownfield & Charpentier, USGS
Analogous Exploratory
Successes
Ceiba Field
Drilled in em 1999 to Triton Energy
Production – 12 mil b/d
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Blocks on Demand
• Paraíba Basin:
5 blocks (SPEPB-AP2)
PB
•Pernambuco Basin:
5 blocks (SPEPB-AP3)
PE
Contractuals
Aspects
Name of Setor
SPEPB-AP2
Exploratory Model
New Frontier
Number of Blocks
5
Area on Demand
~2.300 km²
Exploration Phase
7 years
Exploratory Period
5 + 2 years
Technical Qualification of
the Operator
A
Minimus Bonus
R$ 120 Th. to R$ 290 Th.
Minimum Depth
(Main Objective)
Calumbi Formation (Tertiary) – Blocks 461, 567, 621, 459, 513.
Contractuals
Aspects
Name of the Sector
SPEPB-AP3
Exploratory Model
New Frontier
Number of Blocks
5
Area on Demand
~5.000 km²
Exploration Phase
7 years
Exploratory Period
5 + 2 years
Technical Qualification of
the Operator
Minimum Bonus
Minimum Depth
(Main Objective)
A
R$ 550 Th. a R$ 2.150 Millions
Fm. Calumbi (Tertiary) e/ou Fm. Cabo (Albian) – Blocks 729,
841,785, 896, e 894.
Summary
• Location
• Infraestructure and Operational Conditions
• Exploratory Background
•
Tectono-Stratigraphy Evolution
•
Petroleum Systems
•
Plays
• Analogous Exploratory Sucesses
•
Area on Offer
•
Final remarks
Final remarks
The New Frontier Basin with the presence of structural features /
stratigraphic prominent;
Existence of a western graben (NE-SW), with about 3,500 m of
thickness in the Cupe region with great possibility of the generation of
hydrocarbons;
The "Sub-Basin Plateau“ Pernambuco basin have thicknesses on the
order of 6,000m.
Existence of an evaporite sequence halocinetics and structures that
affect the post-rift sequence.
Final remarks
There is evidence of the existence of a petroleum system (thermogenic)
active in Pernambuco portion of the basin.
The "Sub-Basin Plateau” is the main area potentially generating of HC
in the basin (greater thickness and burial for the syn-rift section).
It is expected a lateral migration to medium / large distance to potential
structural traps present in the High Plateau (mostly in the syn-rift section).
Associated Structures with magmatic features may also be possible
targets for exploration;
Secondly, maybe consider probable stratigraphics traps presents in the
section K upper/ Tertiary age in "Sub-Basin Plateau" (conditioned the
existence of faults).
National Agency of Petroleum, Natural Gas and
Biofuels
Mario de Lima Filho
Contato: [email protected]
www.anp.gov.br