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Goldschmidt2015 Abstracts Timing mismatch between VMS deposits and footwall epidosite alteration in the Semail Ophiolite L. W. DIAMOND1* AND S.GILGEN1 1 Institute of Geological Sciences, University of Bern, Baltzerstrasse 3, CH-3012, Switzerland (*correspondence [email protected]) Epidosites (rocks metasomatically transformed to epidote + quartz + accessory hematite or magnetite) are thought to be products of extreme rock–water interaction and metal leaching deep in hydrothermal convection cells under active spreading ridges in mafic oceanic lithosphere [1] [2]. Discharge of the hydrothermal fluid on the seafloor produces volcanogenic massive sulfide (VMS) deposits. Thus, according to this genetic model, every VMS deposit is under-lain by epidosites at the base of the sheeted-dike complex. The eastern margin of the Semail Ophiolite, Oman, constitutes a tilted section through a thick Sheeted Dike Complex (SDC) overlain by comagmatic ridge-related basalts (Geotimes and Lasail Units), in turn capped by younger suprasubduction zone basalts erupted in a nascent forearc setting (Alley and Boninitic Alley Units [3] [4]). All four volcanic units host VMS deposits [4]. Three small epidosites were previously known in the ophiolite [5], all situated at the base of the SDC in accord with the genetic model. However, our recent field work has identified dozens of other epidosite bodies up to 1 km2 in extent, situated throughout the SDC and the Geotimes and Lasail lavas. Their cross-cutting relations with respect to dated magmatic and tectonic features show that all but one of them formed during the supra-subduction-zone volcanism at 95–94 Ma, some 1.5 Ma after cessation of ridgerelated volcanism and formation of the SDC. The one exceptional epidosite formed during off-axis, transitional latespreading (Lasail) volcanism. Thus, none of the epidosites is demonstrably synchronous with the main oceanic spreading event marked by formation of the SDC and the comagmatic Geotimes lavas, which host abundant VMS deposits. This clear mismatch in timing conflicts with the current genetic model and therefore questions the genetic relationship between footwall epidosites and the source rocks for metals in basalthosted VMS deposits. [1] Richardson et al. (1987) EPSL 84, 243-253. [2] Alt JC (1995) Geophys Monograph 91, Am. Geophys. Union, pp. 85114. [3] Rioux et al. (2013) J. Geophys. Res. Solid Earth 118, 2085-2101. [4] Gilgen et al. (2014) Econ Geol 109: 15851610. [5] Nehlig et al. (1994) J. Geophys. Res. Solid Earth 99(B3), 4703-4713. 729 729 Goldschmidt2015 Abstracts Late Jurassic ocean anoxic event: Evidence from voluminous sulfide deposition and preservation in the Panthalassa Ocean T. NOZAKI12, Y. KATO12 AND K. SUZUKI1 1 R&D CSR/JAMSTEC, 2-15 Natsushima-cho, Yokosuka, Kanagawa 237-0061, Japan ([email protected]) 2 Univ. of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo 113-8656, Japan ([email protected]) Basement rock of the Japanese Island is mainly composed of accretionary complexes since Paleozoic periods. There are several types of ore deposits such as Besshi-type sulfide deposit, Mn carbonate deposit in the bedded chert succession and Mn oxide deposit on seamount basalt, which were derived from seafloor mineralization and are now observed on land. Constituent minerals of Besshi-type sulfide and Mn carbonate deposits are stable under the reducing condition, whereas Mn oxides precipitated contrastingly under the oxic condition. Since the distribution of these three types of deposits is curiously uneven in the Japanese accretionary complexes [1], the redox history of the Panthalassa Ocean might be unraveled based on their depositional ages. The historically productive copper-bearing Besshi-type sulfide deposits in the Japanese accretionary complex were formed as volcanogenic massive sulfide deposits on the deepsea floor of the Panthalassa Ocean. Here we report that eleven typical Besshi-type deposits yielded Re-Os isochron ages around 150 Ma (148.4 ± 1.4 Ma from the composite isochron) in Late Jurassic time [2] [3]. This date coincides with the lowest marine 87Sr/86Sr ratio and highest atmospheric CO2 concentration of the past 300 million years. We infer that intense mid-ocean ridge hydrothermal and volcanic activity in the Late Jurassic produced huge sulfide deposits and large emissions of CO2 gas, leading to global warming and a stratified Panthalassa Ocean with anoxic deep seas that favored preservation of sulfides in the pelagic environment. The emergence of ocean anoxia triggered by seafloor volcanism is also consistent with a positive δ13C excursion and widespread deposition of petroleum source rocks and black shales. [1] Sato, K. and Kase, K. (1996) Island Arc, 5, 216-228. [2] Nozaki, T. et al. (2010) Geochim. Cosmochim. Acta, 74, 43224331. [3] Nozaki, T. et al. (2013) Sci. Rep., 3, 1889, doi: 10.1038/srep01889. 2301 2301 Goldschmidt2015 Abstracts Pyrite Re-Os geochronology: Lessons from the Irish orefield D. HNATYSHIN1*, R. A. CREASER1, J. J. WILKINSON2, R. A. STERN1 AND S. A. GLEESON1 1 Department of Earth & Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada (*[email protected], [email protected], [email protected], [email protected]) 2 Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK ([email protected]) The Irish Zn-Pb orefield is one of the world’s largest hydrothermal Zn-Pb ore districts, but uncertainty in the timing of mineralization made distinguishing between different potential genetic models for ore formation difficult. Three main proposals for the timing of mineralization have been suggested. The first model is that the deposits formed in the shallow subsurface shortly after or during deposition of the host rocks (~350Ma). The second is that these deposits formed after significant burial (<340Ma), and the third is that they formed during the Variscan orogeny (310-290 Ma). Distinguishing between these different possibilities is possible using pyrite Re-Os isochron methods. Hnatyshin et al. (2015) [1] determined robust Re-Os ages for the Lisheen Main Zone (346.6 ± 3.0 Ma, MSWD = 1.6 ) and the Silvermines B-zone (334 ± 6.1 Ma, MSWD = 19). However, some pyrite samples fromt the Irish deposits produced isochrons that show a greater amount of complexity. In particular, the high quality results produced by the Lisheen Main Zone are not replicated using samples from the Lisheen Bog Zone. Whereas a very similar age is produced (345 ± 11 Ma) the scatter in the data is much higher (MSWD = 80). To determine the source of the scatter a variety of different techniques were used to characterize both sets of samples, including petrographic imaging, back-scattered electron imaging, trace element mapping, in-situ sulfur isotope measurements, as well as acid leaching experiments. The results show that the Bog Zone samples contain a much more complicated suite of intergrown sulphide minerals and contain multigenerational pyrite showing distinct textural and chemical differences, likely resulting in the excess scatter observed in the Re-Os data. Ultimately, these results suggest that screening out excessively complicated samples is required when trying to produce precise and accurate ages using pyrite Re-Os geochronology. [1] Hnatyshin. et al. 2015, Geology, v. 43, p. 143-146. 1278 1278 Goldschmidt2015 Abstracts Re-Os age of late bornite-chalcopyrite vein ores, Kupferschiefer, SW Poland S. Z. MIKULSKI1 AND H. J. STEIN23 1 Mineral Resources Program, Polish Geological Inst. National Research Inst., Poland (stanislaw.mikulski @pgi.gov.pl) 2 AIRIE Program, Colorado State University, USA ([email protected]) 3 CEED, University of Oslo, 0316 Oslo, Norway The age of the world-class Cu-Ag stratabound mineralization from the southern margin of the Upper Zechstein basin in Poland has been addressed using different geochronological methods. In general the ages of the Kupferschiefer’s mineralized samples span from Lower Triassic to Lower Cretaceous [1] [3-5] [7-8]. Economic Cu mineralization transgresses sedimentary sequences and is hosted by Kupferschiefer black shale, underlying sandstone (Rotliegendes) and overlapping limestone of the Upper Permian marine sequence (lower Zechstein). Cu-Ag ores are represented mainly by Cu sulphides such as chalcocite, bornite, chalcopyrite and covellite which are commonly associated with silver admixtures and/or minerals. Four samples from the Lubin (-610 m b.s.l.) and Polkowice (-740 m b.s.l.) operating mines were acquired for Re-Os analyses. Analyzed samples consist of economic Cu ores characterized by 1-10 mm bornite ± chalcopyrite veinlets in calcareous shale (5-10 cm thick) rich in organic matter. In any single veinlet, bornite and chalcopyrite may occur in variable proportion, and penetrate along shale laminations as fine-grained (1-30 μm in diameter) disseminations and small aggregates (<50 µm). Within macroscopic veinlets where chalcopyrite is present, it forms symmetrical margins to a bornite interior. Bornite, bornitechalcopyrite and/or chalcopyrite veinlets may cross-cut bedding or be nearly parallel to lamination in black shales. We report a Re-Os isochron age for bornite ± chalcopyrite veinlets that exhibit shallow cross-cutting features to bedding in black shale. A Model 1 regression yields 212 ± 7 Ma, with an initial 187 Os/188Os ratio of 2.13 ± 0.31 (MSWD = 1.3). The analyzed bornite ± chalcopyrite veinlets have a Re concentration ranging from 5.7 to 12.1 ppb, and a total Os concentration ranging from 27-52 ppt. Significant common Os is present in all of the analyzed samples. The current Model 1 age suggests a higher initial 187Os/188Os than our previous result [4]. The origin of the Kupferschiefer mineralization is commonly attributed to multiple flow events of low-temperature oxidizing metalliferous fluids triggered by tectonic activation of basinal sediments (e.g. [2] [6]). Our results strongly suggest that the main Cu-mineralization event took place in the Late Triassic (Norian), ca. 212 ± 7 Ma. The work was supported by grant No. N525 393739 from the Ministry of Science and Higher Education to SM. [1] Bechtel et al. (1999) Econ. Geol. 94, 261 [2] Blundell et al. (2003) Econ. Geol. 98, 1487. [3] Jowett et al. (1987) J. Geophys. Res. 92, 581. [4] Mikulski and Stein (2010) GCA, A708. [5] Nawrocki (2000) Econ. Geol. 95, 241. [6] Oszczepalski (1999) Min. Deposita 34, 599. [7] Pasava et al. (2007a) GCA, A763. [8] Pasava et al. (2010) Min. Deposita 45, 189. 2129 2129 Goldschmidt2015 Abstracts Multiple IOCG-forming events in the Carajás Province, Brazil CAROLINA P. N. MORETO1*, LENA V. S. MONTEIRO2, ROBERTO P. XAVIER1, GUSTAVO H. C. MELO1, MARCO A. DELINARDO DA SILVA1 AND ROBERT A. CREASER3 1 Geoscience Institute, University of Campinas, Rua João Pandiá Calógeras 51, Campinas, Brazil (*correspondence: [email protected]) 2 Geoscience Institute, University of São Paulo, Rua do Lago 562, São Paulo, Brazil 3 Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB T6G 2E3, Canada World-class iron oxide-copper-gold (IOCG) deposits (e.g., Sossego, Salobo, Igarapé Bahia) comprise the most important Cu resources in the Carajás Province, Brazil. The deposits are hosted by: i) Mesoarchean granites, gneisses and greenstone belts; and ii) Neoarchean metavolcanic-sedimentary units, bimodal intrusive rocks and gneisses. Isotope data combined with field evidence suggest a multistage evolution of IOCG mineralization in the Carajás Province, with recurrence of ore-forming systems during the Neoarchean and the Paleoproterozoic. These included: i) Syngenetic to diagenetic chalcopyrite associated with rhythmites at the Igarapé Bahia deposit, and fluid circulation at the Bacuri deposit at 2.76 Ga; ii) A major episode of IOCG formation at 2.72-2.68 Ga related to basin inversion coupled with Neoarchean magmatism (e.g., Sequeirinho-Pista ore bodies at the Sossego deposit; Bacaba, Castanha, Bacuri, Visconde and Cristalino deposits); iii) A ca. 2.5-2.4 Ga hydrothermal and/or remobilization events synchronous with shear zone reactivation and responsible for the Sabolo and Igarapé Bahia deposits; iv) Paleoproterozoic (1.90-1.87 Ga) IOCG mineralization related to the emplacment of A-type granites and represented by the Sossego-Curral ore bodies (Sossego deposit) and the Alvo 118 deposit. The deep-seated Neoarchean IOCG systems are characterized by breccia and replacement bodies associated with albite–scapolite, biotite–scapolite–tourmaline or almandine–grunerite, and magnetite– (apatite–actinolite) formation. Shallow-emplaced Paleoproterozoic IOCG systems, formed under brittle-dominated regime, have characteristic potassic and chlorite alteration zones. The reccurence of hydrothermal systems in time and space contributed to the complex hydrothermal overprint observed in the Neoarchean deposits, as well as Cu enrichment in the Paleoproterozoic. 2191 2191 Goldschmidt2015 Abstracts High spatial resolution SHRIMP and LA-ICPMS U-Pb geochronology of Pea Ridge Fe-REE-Au deposit, USA L. A. NEYMARK1, J. N. ALEINIKOFF2, C. S. HOLM-DENOMA3, A. J. PIETRUSZKA4, R. M. PILLERS5 AND R. J. MOSCATI6 1 [email protected] [email protected] 3 [email protected] 4 [email protected] 5 [email protected] 6 [email protected] 2 Precise and accurate determination of the timing and duration of ore-forming processes is crucial for understanding the origin of deposits and placing them in a regional geologic context. The Pea Ridge iron oxide - apatite deposit in the ~1.47-1.44 Ga St. Francois Mountains terrane, southeast Missouri, USA is an endmember type in the global spectrum of iron oxide – copper - gold deposits. Abundant monazite and xenotime occur in REE-rich breccia pipes that cut the host rhyolite, magnetite ore, and alteration zones associated with the iron ore system. As revealed by CL and BSE imagery, most dateable minerals from this deposit are intergrown in a fine-grained matrix, or have numerous inclusions and/or overgrowths, thereby requiring high spatial resolution geochronology to obtain accurate age constraints on ore formation. SHRIMP U-Pb zircon ages of 1473.6 ± 8.0 (2σ) and 1472.7 ± 5.6 Ma were obtained for the host rhyolite. Two dissolved bulk apatite samples from magnetite ore yielded TIMS upper intercept ages of 1461.3±8.3 and 1466.2±4.0 Ma and showed normal age discordance due to minor Pb loss. Micron-sized equant monazite inclusions in the apatite yielded a LA-ICPMS age of 1442±12 Ma. LA-ICPMS analysis of inclusion-free portions of pyrite (with U/Pb~0) from magnetite ore yield high radiogenic Pb isotopic values (206Pb/204Pb up to 60), indicating redistribution of Pb during a process that was likely much younger than 1.4 Ga. Monazite and xenotime in the REE-rich breccia pipes have variable morphologies, but yielded nearly identical SHRIMP ages of 1462.5 ± 1.5 and 1462.7 ± 9.3 Ma, respectively. Although textural evidence suggests the possibility of multiple hydrothermal events, better analytical precision than is currently achieved by LA-ICPMS and SHRIMP is required to resolve potential age variability at a finer time scale. However, our high spatial resolution dating results indicate that the hydrothermal activity responsible for mineralization at the Pea Ridge deposit post-dated volcanism by up to 10 Ma and lasted for tens of millions of years. 2264 2264 Goldschmidt2015 Abstracts Temporal constraints on magma dynamics resulting in porphyry copper deposit formation S. TAPSTER1*, D. J. SMITH2, J. A. NADEN3 AND D. J. CONDON1 1 NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham, NG12 5GG, U.K. *correspondence: [email protected]) 2 Department of Geology, University of Leicester, University Road, Leicester, LE1 7RH, U.K 3 British Geological Survey, Keyworth, Nottingham, NG12 5GG, U.K. The timing and duration of volatile exsolution repsonsible for porphyry-style copper mineralisation are ultimately controlled by the dynamics within the long-lived magmatic systems that supply the metals and ore-forming fluids. Volatile saturation occurs in response to changes in pressure, temperature and crystallinity of the source magma. We examine the temporally constrained relationships between mineralisation and magma dynamics at depth in one of the world’s youngest exposed porphyry systems, the Koloula Poprhyry Prospect, Solomon Islands. Geological relationships and high precision ID-TIMS U-Pb zircon dating constrain assembly of the shallow level pluton to <150 kyr. Mineralising poprhyry intrusions followed within ca. 50 kyr. Discrete mineralising intrusive events are separated by 34 ± 24 kyr, also constraining the duration of the first, oreforming hydrothermal event. Dates define both protracted zircon crystallisation at depth and rapid recycling to the crustal level of porphyries. We apply a multifaceted approach combining: textural analysis of zircons; U-Pb geochronology; Ti-in zircon thermometry; and geochemical modelling of zircon dissolution rates and magma crystallinity-temperature relationships for suitable approximations of conditions in the underlying plutonic system. Results show that magmas resided in a highly crystallised (>50%), volatile saturated, immobile state for extended periods at depth preceeding porphyry formation. Liberated mobile melt fractions that transported the requisite components for mineralisation to shallow levels were transient, existing for <10–20 kyr. Intrusion of andesitic magmatism under the highly crystallised silicic pluton provided the energy for thermal rejuvenation. Porphyry formation was likely promoted by rejuvenation following the addition and percolation of hot volatiles, during low fluxes of andesitic magma; rather than extensive magma mixing, which occurred during high fluxes. 3079 3079 Goldschmidt2015 Abstracts Duration of ore formation: Grasberg porphyry copper deposit, Papua, Indonesia S. WAFFORN1*, M. CLOOS1 AND D. F. STOCKLI1 1 University of Texas at Austin, Austin, TX 78713 *correspondance: [email protected] Isotopic dating of intrusions and hydrothermal alteration from porphyry copper deposits worldwide is rarely able to constrain the duration of ore formation with a resolution better than one million years. Zircon U/Pb dating of intrusions that host and cross-cut ore grade mineralization at the supergiant Grasberg deposit, located in Papua, Indonesia, provides a constraint on the maximum duration of hydrothermal fluid flow. Porphyry copper-type mineralization is hosted in the Grasberg Igneous Complex (GIC), which comprises three pulses of magmatism: the Dalam Phase, the Main Grasberg Intrusion (MGI), and the Kali Dikes. Main phase copper mineralization initiated following intrusion of the MGI (3.07±0.05 Ma, n=107) and predates the Late Kali Dike (2.99±0.05 Ma, n=90). Based on these ages the Grasberg deposit formed in less than 180 k.y, and perhaps less than 80 k.y. The oldest intrusion dated in the Ertsberg-Grasberg district is the Wanagon Sill (3.43±0.07 Ma, n=52) and the youngest intrusion is a dike cutting the Ertsberg pluton (2.71±0.07 Ma, n=32). These data constrain the duration of magmatism in the district to less than 900k.y. Apatite and zircon (U-Th)/He (aHe and ZHe) ages provide additional insight into the low-temperature thermal history associated with ore formation. Samples were collected from a vertical profile in the Kali Dikes spanning 2 km. Near-surface samples cooled almost immediately following crystallization (3.1±0.2 Ma zHe age), whereas samples at 2 km depth cooled more slowly (2.1±0.3 Ma zHe age). Throughout the vertical profile aHe ages are less 0.6 m.y. younger than the than the zHe ages. Based on these ages the calculated cooling rate from 750-180°C was 150°C/10 k.y. near the surface, 11°C/10 k.y. at 1 km depth, and 4°C/k.y. at 2 km depth. The cooling rate from 180-70°C was 11°C/k.y. Collectively these results indicate Grasberg ore formation occurred immediately following MGI emplacement, was short-lived, and the system rapidly cooled. The high cooling rates to temperatures below 70°C at 2 km depth indicate the wall rock was cold and preclude the presence of a 2 km tall volcanic structure over the orebody. High cooling rates and steep thermal gradients along the edges of the stock would cause rapid deep-seated crystallization of quartz and feldspars. This led to the formation of copper-rich fluid bubbles in mobile magma that rose to collect beneath a cupola before ascending to form the Grasberg orebody. 3297 3297 Goldschmidt2015 Abstracts Using zircon petrochronology to constrain timescales of porphyry Cu formation: an example from Bajo de la Alumbrera, NW Argentina Y. BURET1*, A. VON QUADT1, C. A. HEINRICH1 AND I. PEYTCHEVA12 1 Department of Earth Sciences, Institute of Geochemistry and Petrology, ETH Zurich, Switzerland (*correspondence: [email protected]) 2 Bulgarian Academy of Science, Geological Institute, Sofia, Bulgaria. Using high-precision U-Pb dating we are able to determine timescales of porphyry emplacement and ore formation. Previous studies have suggested timescales of porphyry Cu formation ranging from <100 yr [1], to as much as 1 Ma [2]. In contrast recent numerical simulations suggest Cu precipitation occurs in the range of 50-100 ka [3]. Therefore in order to better constrain timescales of porphyry Cu formation, we apply high precision U-Pb zircon geochronology to estimate porphyry emplacement ages. Furthermore, high precision zircon U-Pb dates combined with trace element and Hf isotope analyses of zircons can provide useful insights into upper crustal magmatic processes which immediately precede the formation of porphyry Cu deposits. This study focuses on the ~7 Ma Bajo de la Alumbrera CuAu deposit, NW Argentina. The deposit consists of a composite stock of dacitic porphyries. The relative timing of each porphyry intrusion is established based on clear crosscutting field relationships between different porphyry intrusions, which include the pre-mineralisation P2 porphyry, pre-syn-minerlisation EP3 porphyry, and the postmineralisation LP3 and P4 porphyries. Single zircon crystals from individual porphyry intrusions (P2, EP3, LP3, P4) in the Alumbrera deposit have been dated using CA-ID-TIMS, employing the ET2535 tracer solution for maximum precision and accuracy. All porphyries display protracted zircon crystal growth over 100-200 ka timescales. Using the youngest zircon population from each of the porphyry intrusions, we conclude that Cu mineralisation occurred on 10 ka timescales, similar to those proposed by recent numerical predictions [3]. Trace element analyses from the dated zircons suggest that all of the dated porphyries are derived from the same body of underlying magma and show non-systematic trace element and εHf trends with time. [1] Cathles and Shannon (2007) EPSL 262: 92-108. [2] Ballard et al. (2001) Geology 29: 383-386. [3] Weis et al. (2012) Science 338: 1613-1616. 425 425 Goldschmidt2015 Abstracts Cooling and mineralisation history of Karakartal porphyry system, Erzincan, Turkey OĞUZHAN GÜMRÜK1*, MIĞRAÇ AKÇAY1, NESLIHAN ASLAN1, BRENT MCıNNES2, NOREEN EVANS2 2 AND FRED JOURDAN 1 Karadeniz Technical University, Trabzon, Turkey John de Laeter Centre, Curtin University, Perth, Western Australia (*correspondence: [email protected]) 2 The Karakartal porphyry deposit is located near the Kabataş village (Kemaliye-Erzincan) in a metallogenic zone covering Divriği (Sivas)-İliç-Kemaliye (Erzincan) and Tunceli provinces of east central Anatolia. The region has a complex geological setting with the presence of Mesozoic to Tertiary rocks. Early-Middle Eocene subvolcanic rocks (SVR) intrude Jurasic-Crataceous limestones and Early Eocene clastic and volcanic rocks. Field observations on cross-cutting relationships between magmatic phases show at least four (preand syn- mineralization, post mineralization dykes and post mineralization volcanic rocks) different magmatic episodes. These magmatic phases have gabbroic to granodioritic compositions and are geochemically similar to volcanic arc granites. This study aims at exhibiting mineralisation and cooling history of the Karakartal porphyry system based on U-Pb, Ar/Ar and U-Th/He geochronology. Zircon U-Pb data from SVRs, (potassicly altered) syn-mineralization- and postmineralization dykes, and post mineralization basalts indicate emplacement ages of 49.2±1.5 Ma, 45.81±0.44 Ma and 43.2±1.2 Ma, respectively. Ar/Ar ages from biotites and Kfeldspars of K-silicate alteration are determined to be 49.86±0.32 Ma and 47.32±0.57 Ma, respectively. (U-Th)/He thermochronology on zircons from potassicly altered SVR’s, however, give an age data of 45.8±0.8 Ma. These age constraints from magmatic rocks and potassic alteration zones within them indicate that magmatism was initiated in the region at around 50 Ma and continued till around 43 Ma, lasting for around 7 Ma. Commencement of porphyry system is nearly coeval with the initial magmatism and went on till about 45 Ma, characterised by zircon thermochronology. This project was financially supported by the Turkish Science Foundation (Tübitak) through the 110Y308 project. 1122 1122 Goldschmidt2015 Abstracts The optimal pathways leading to earthquake-enhanced gold precipitation in the epithermal environment P. SÁNCHEZ-ALFARO12*, M. REICH12, T. DRIESNER3, G. ARANCIBIA24, P. PÉREZ-FLORES24, J. CEMBRANO24, J. ROWLAND5 AND C. HEINRICH3 1 Dept. of Geology, Universidad de Chile, Santiago, Chile (*correspondence: [email protected]) 2 Andean Geothermal Center of Excellence (CEGA), Universidad de Chile, Santiago 3 ETH Zürich, Isotope Geochemistry and Mineral Resources, Zürich, Switzerland 4 Dept. of Structural Engineering, Pontificia Universidad Católica de Chile, Santiago, Chile 5 School of Environment, The University of Auckland, Auckland, New Zealand Hydrothermal ore deposits result from the combination of a sustained flux of metal-rich fluids and an efficient precipitation mechanism. Earthquakes may trigger gold precipitation in the epithermal environment but its efficiency and time-integrated contribution is poorly quantified. In order to quantify the feedbacks between earthquakedriven fracturing and metal precipitation in the shallow crust, we have constrained the past and present physico-chemical conditions of a geothermal system in the highly seismic Chilean Andes. We combined temperature measurements in the deep wells with geochemical analyses of fluid samples retrieved from the reservoir. In addition, we reconstructed the paleo-fluid conditions using microthermometry and LA-ICPMS data of fluid inclusions from a deep borehole core. The effect of pressure and enthalpy changes on precipitation was evaluated by calculating the solubility of Au in P-H space, and the impact of externally-forced, seismic perturbations on fluid parameters was constrained using a thermo-mechanical piston model for a “suction pump” mechanism. The reconstructed PT-H-X fluid trajectories indicate that fluids feeding the hydrothermal reservoir reach boiling conditions with a high gold budget (~1-5 ppb) at saturated liquid pressures between 50 and 120 bar. Our results show that if hydrothermal ore fluids reach this optimal threshold for metal precipitation, small adiabatic pressure changes (~50 bar) triggered by transient fault-rupture can drop gold solubility by up to two orders of magnitude. We conclude that such externally-forced perturbations, equivalent to low magnitude earthquakes (Mw<2) significantly enhance gold precipitation efficiency. 2750 2750 Goldschmidt2015 Abstracts Hydrological and geological constraints on timescales of magmatic-hydrothermal ore deposits PHILIPP WEIS12 1 Institute of Geochemistry and Petrology, ETH Zurich, Switzerland ([email protected]) 2 GFZ Potsdam, Germany Chemical enrichment of metals in magmatic-hydrpthermal ore deposits majorly depends on the physical hydrology of fluids flowing through rocks. The respective geological setting and associated physical hydrology play a decisive role in forming distinct ore deposit types, including volcanogenic massive sulfide deposits at mid-ocean ridges or submarine arc volcanos, porphyry deposits in continental arcs, and epithermal deposits. Simulation results from a numerical process model for thermohaline convection in conjunction with a dynamic permeability model are used to constrain the timescales of ore formation. Thermal convection, volatile expulsion, and saltwater dynamics are first-order hydrological components with different intrinsic timescales, and different combinations or successions of these general patterns can help to constrain the timing and duration of particular ore-forming systems. The physical behavior of hydrothermal systems can be counterintuitive, because of the nonlinear properties of fluids and rocks as a function of pressure, temperature and composition. In porphyry copper systems, mineralization is localized by a self-stabilizing hydrological front, located at the transition from brittle to ductile rock behavior and controlled by the heat balance between an external convective cooling engine and an overpressured magmatic fluid plume. Above this hydrological divide, magmatic and meteoric fluids mix on ascent to the surface, providing a mechanism for the transition from porphyry to epithermal deposits. In mid-ocean ridge hydrothermal systems, focused warm downflow in the immediate vicinity of hot upflow zones may be a more efficient mechanism for metal leaching than broad-scale lateral infiltration of seawater, promoting ore-formation in Cyprustype massive sulfide deposits. In submarine magmatichydrothermal systems, phase separation can lead to a decoupling of vapor-dominated venting during relatively short periods of magmatic fluid expulsion, leading to the formation of Au-rich chimneys, and brine-dominated venting during convection in an extended waning stage, leading to the formation of base-metal deposits. All simulations of magmatic-hydrothermal ore formation indicate timescales in the order of a few 102 to 105 years for single mineralization events. 3382 3382