Genesis of the world-class Dachang gold deposit, Northern Qinghai-Tibet Plateau: A multiproxy approach
暂无分享,去创建一个
Ling Zhang | Yehui Zhang | Mamta Santosh | W. Zhai | Jinlong Liang | E. Zhang | Junkang Zhao | Song-yan Han | Silun Zheng | Feng Yang | Xiao Ming Sun | Canyun Liao | Xiao-ming Sun
[1] Xiaoming Sun,et al. In situ pyrite sulfur isotope and trace element analyses of the world-class Dachang gold deposit, northern Qinghai-Tibetan Plateau: Implications for metallogenesis , 2021 .
[2] D. Alderton. Fluid Inclusions , 2021, Encyclopedia of Geology.
[3] Xiaoming Sun,et al. Fluid Inclusions and Stable Isotopic Characteristics of the Yaoling Tungsten Deposit in South China: Metallogenetic Constraints , 2018, Resource Geology.
[4] A. Zotov,et al. Stability of AuCl2− from 25 to 1000 °C at Pressures to 5000 bar and Consequences for Hydrothermal Gold Mobilization , 2018, Minerals.
[5] Hejing Wang,et al. Tectonothermal evolution of the Triassic flysch in the Bayan Har Orogen, Tibetan plateau , 2018 .
[6] Yunpeng Dong,et al. Subduction and accretionary tectonics of the East Kunlun orogen, western segment of the Central China Orogenic System , 2017, Earth-Science Reviews.
[7] L. Ding,et al. Pre-Cenozoic geologic history of the central and northern Tibetan Plateau and the role of Wilson cycles in constructing the Tethyan orogenic system , 2016 .
[8] K. Grice,et al. Associations between sulfides, carbonaceous material, gold and other trace elements in polyframboids: Implications for the source of orogenic gold deposits, Otago Schist, New Zealand , 2016 .
[9] Xiaoming Sun,et al. Fluid inclusion geochemistry and Ar–Ar geochronology of the Cenozoic Bangbu orogenic gold deposit, southern Tibet, China , 2016 .
[10] Xiaoming Sun,et al. Geology, geochemistry, and genesis of orogenic gold–antimony mineralization in the Himalayan Orogen, South Tibet, China , 2014 .
[11] D. Gaboury. Does gold in orogenic deposits come from pyrite in deeply buried carbon-rich sediments?: Insight from volatiles in fluid inclusions , 2013 .
[12] A. Tomkins. On the source of orogenic gold , 2013 .
[13] Hejing Wang,et al. Tectonothermal evolution of the Triassic flysch in the Songpan-Garzê orogen, eastern Tibetan plateau , 2013 .
[14] F. Sun,et al. Origin of the Dachang gold deposit, NW China: constraints from H, O, S, and Pb isotope data , 2013 .
[15] Yong‐Fei Zheng,et al. Tectonic evolution of a composite collision orogen: An overview on the Qinling–Tongbai–Hong'an–Dabie–Sulu orogenic belt in central China , 2013 .
[16] Wu Bo. Geochemistry,zircon LA-ICP-MS U-Pb dating and geological significance of Zharijia granitoids in Dachang area,Qinghai Province , 2013 .
[17] Wang Chang. The genesis of the Dachang gold ore field in Qinghai Province: Constraints on fluid inclusion geochemistry and H-O isotopes , 2013 .
[18] Liu Han-bi. Determination of stable isotope composition in uranium geological samples , 2013 .
[19] P. Burnard,et al. Noble gases and halogens in fluid inclusions: A journey through the Earth's crust , 2013 .
[20] Robert J. Bodnar,et al. HokieFlincs_H2O-NaCl: A Microsoft Excel spreadsheet for interpreting microthermometric data from fluid inclusions based on the PVTX properties of H2O-NaCl , 2012, Comput. Geosci..
[21] Xiaoming Sun,et al. He-Ar isotope geochemistry of the Yaoling-Meiziwo tungsten deposit, North Guangdong Province: Constraints on Yanshanian crust-mantle interaction and metallogenesis in SE China , 2012 .
[22] Yongxin Pan,et al. New 40Ar/39Ar dating results from the Shanwang Basin, eastern China: Constraints on the age of the Shanwang Formation and associated biota , 2011 .
[23] R. Large,et al. A Carbonaceous Sedimentary Source-Rock Model for Carlin-Type and Orogenic Gold Deposits , 2011 .
[24] N. Oliver,et al. The noble gas systematics of late-orogenic H2O–CO2 fluids, Mt Isa, Australia , 2011 .
[25] R. Berry,et al. Pyrite and Pyrrhotite Textures and Composition in Sediments, Laminated Quartz Veins, and Reefs at Bendigo Gold Mine, Australia: Insights for Ore Genesis , 2011 .
[26] A. Zotov,et al. Thermodynamic description of aqueous species in the system Cu-Ag-Au-S-O-H at temperatures of 0–600°C and pressures of 1–3000 bar , 2010 .
[27] J. Malavieille,et al. The tectonic evolution of the Songpan-Garzê (North Tibet) and adjacent areas from Proterozoic to Present: A synthesis , 2010 .
[28] A. Tomkins. Windows of metamorphic sulfur liberation in the crust: Implications for gold deposit genesis , 2010 .
[29] Ding Qing. Ore-forming fluid evolution of Dachang gold deposit in Qumalai County, Qinghai Province: Evidence from fluid inclusion study and arsenopyrite geothermometer , 2010 .
[30] Nigel J. Cook,et al. Metallogenesis of the Tibetan collisional orogen: A review and introduction to the special issue , 2009 .
[31] R. Large,et al. Gold and Trace Element Zonation in Pyrite Using a Laser Imaging Technique: Implications for the Timing of Gold in Orogenic and Carlin-Style Sediment-Hosted Deposits , 2009 .
[32] R. Powell,et al. Formation of gold deposits: Review and evaluation of the continuum model , 2009 .
[33] Zhao Cai. A discussion on geological characteristics and genesis of Dachang gold deposit in Qinghai Province , 2009 .
[34] Liu Jian-xian. Raman spectroscopic characteristics of bitumen inclusions , 2009 .
[35] Li Shi-jin. Study on Forming Conditions and Metallogenesis of Kuhai Mercury Deposit,Qinghai Province , 2009 .
[36] P. Vasconcelos,et al. Structural and geochronological constraints on the tectono-thermal evolution of the Danba domal terrane, eastern margin of the Tibetan plateau , 2008 .
[37] G. Gehrels,et al. Cenozoic tectonic evolution of Qaidam basin and its surrounding regions (Part 1): The southern Qilian Shan-Nan Shan thrust belt and northern Qaidam basin , 2008 .
[38] A. Yin,et al. Cenozoic tectonic evolution of the Qaidam basin and its surrounding regions (Part 3): Structural geology, sedimentation, and regional tectonic reconstruction , 2008 .
[39] G. Gehrels,et al. Mediterranean-style closure of the Paleo-Tethys ocean , 2008 .
[40] A. Weislogel. Tectonostratigraphic and geochronologic constraints on evolution of the northeast Paleotethys from the Songpan-Ganzi complex, central China , 2008 .
[41] J. Malavieille,et al. Tectonic evolution of the Triassic fold belts of Tibet , 2008 .
[42] K. F. Cassidy,et al. Granitoid-associated orogenic, intrusion-related, and porphyry style metal deposits in the Archean Yilgarn Craton, Western Australia , 2007 .
[43] Li Da-xin. Fluid inclusions in orogenic gold deposits in the northern Qaidam margin-East Kunlun region , 2007 .
[44] Sha Shuqing. Zircon SHRIMP Dating and Geochemical Characteristics of Granites in the Eastern Part of the Bayan Har Mountains , 2007 .
[45] D. Craw,et al. Sources of Metals and Fluids in Orogenic Gold Deposits: Insights from the Otago and Alpine Schists, New Zealand , 2006 .
[46] N. Harris,et al. U Pb zircon SHRIMP ages, geochemical and Sr Nd Pb isotopic compositions of intrusive rocks from the Longshan Tianshui area in the southeast corner of the Qilian orogenic belt, China: Constraints on petrogenesis and tectonic affinity , 2006 .
[47] Lei Yu-hong. The Basement of Baryan Har Basin Is A Part of Western Yangtze Platform: Evidence from Granites , 2006 .
[48] A. Yin,et al. Structural evolution of the Yushu-Nangqian region and its relationship to syncollisional igneous activity, east-central Tibet , 2005 .
[49] R. Handler,et al. 40Ar/39Ar mineral ages from basement rocks in the Eastern Kunlun Mountains, NW China, and their tectonic implications , 2005 .
[50] Zhao Cai-sheng,et al. Fluid inclusion characteristics of Dachang gold deposit, Qinghai Province and their geological significance , 2005 .
[51] Zhang De-quan. Ar-Ar dating of orogenic gold deposits in northern margin of Qaidam and East Kunlun Mountains and its geological significance , 2005 .
[52] Albert H. Hofstra,et al. Carlin-Type Gold Deposits in Nevada: Critical Geologic Characteristics and Viable Models , 2005 .
[53] A. Leipertz,et al. A study of the Raman spectra of alkanes in the Fermi-resonance region , 2004 .
[54] D. Zheng,et al. Onset timing of significant unroofing around Qaidam basin, northern Tibet, China: constraints from 40Ar/39Ar and FT thermochronology on granitoids , 2004 .
[55] M. L. Miller,et al. The Late Cretaceous Donlin Creek Gold Deposit, Southwestern Alaska: Controls on Epizonal Ore Formation , 2004 .
[56] P. Burnard,et al. Importance of mantle derived fluids during granite associated hydrothermal circulation: He and Ar isotopes of ore minerals from Panasqueira , 2004 .
[57] F. Cheng. Geochemical characteristics of ore-forming fluids from the orogenic Au(and Sb)deposits in the eastern Kunlun area,Qinghai province , 2004 .
[58] J. Malavieille,et al. Timing of granite emplacement and cooling in the Songpan–Garzê Fold Belt (eastern Tibetan Plateau) with tectonic implications , 2004 .
[59] L. Ratschbacher,et al. Subduction, collision and exhumation in the ultrahigh-pressure Qinling-Dabie orogen , 2004, Geological Society, London, Special Publications.
[60] P. O'Brien,et al. Exhumation of early Tertiary, coesite-bearing eclogites from the Pakistan Himalaya , 2003, Journal of the Geological Society.
[61] L. Ratschbacher,et al. Tectonics of the Qinling (Central China): tectonostratigraphy, geochronology, and deformation history , 2003 .
[62] F. Robert,et al. Gold Deposits in Metamorphic Belts: Overview of Current Understanding,Outstanding Problems, Future Research, and Exploration Significance , 2003 .
[63] N. Harris,et al. The Tertiary collision‐related thermal history of the NW Himalaya , 2002 .
[64] K. J. Schmidt,et al. UV Raman Spectroscopy of Oilsands-Derived Bitumen and Commercial Petroleum Products , 2002 .
[65] T. Baker. EMPLACEMENT DEPTH AND CARBON DIOXIDE-RICH FLUID INCLUSIONS IN INTRUSION-RELATED GOLD DEPOSITS , 2002 .
[66] X. Bi,et al. Geology and geochemistry of Carlin-type gold deposits in China , 2002 .
[67] Lijuan Wang,et al. Determining gaseous composition of fluid inclusions with quadrupole mass spectrometer , 2002 .
[68] P. Burnard,et al. Production, Release and Transport of Noble Gases in the Continental Crust , 2002 .
[69] J. Malavieille,et al. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau: fission-track constraints , 2001 .
[70] D. Groves,et al. Orogenic gold and geologic time: a global synthesis , 2001 .
[71] P. Kamp,et al. Tectonics and denudation adjacent to the Xianshuihe Fault, eastern Tibetan Plateau: Constraints from fission track thermochronology , 2000 .
[72] A.,et al. A Comparison of Australian and Global Examples , 2000 .
[73] F. Bierlein,et al. Phanerozoic orogenic lode gold deposits , 2000 .
[74] P. E. Brown,et al. Characteristics and models for carlin-type gold deposits , 2000 .
[75] K. F. Cassidy,et al. Archean orogenic lode gold deposits , 2000 .
[76] P. E. Brown,et al. Exploration for epithermal gold deposits , 2000 .
[77] J. Jehlička,et al. First and second order Raman spectra of natural highly carbonified organic compounds from metamorphic rocks , 1999 .
[78] P. Burnard,et al. Mantle, crustal and atmospheric noble gases in ailaoshan gold deposits, Yunnan Province, China , 1999 .
[79] T. McCuaig,et al. P—T—t—deformation—fluid characteristics of lode gold deposits: evidence from alteration systematics , 1998 .
[80] E. Mikucki. Hydrothermal transport and depositional processes in Archean lode-gold systems: A review , 1998 .
[81] Richard J. Goldfarb,et al. Orogenic gold deposits : A proposed classification in the context of their crustal distribution and relationship to other gold deposit types , 1998 .
[82] D. Kontak,et al. An isotopic (C, O, Sr) study of vein gold deposits in the Meguma Terrane, Nova Scotia; implication for source reservoirs , 1997 .
[83] D. Graham,et al. Resolving lithospheric and sub-lithospheric contributions to helium isotope variations in basalts from the southwestern US , 1996 .
[84] F. Stuart,et al. Resolving mantle and crustal contributions to ancient hydrothermal fluids: HeAr isotopes in fluid inclusions from Dae Hwa WMo mineralisation, South Korea , 1995 .
[85] Tibor J. Dunai,et al. Helium, neon, and argon systematics of the European subcontinental mantle: Implications for its geochemical evolution , 1995 .
[86] X. Gu. Geochemical characteristics of the Triassic Tethys-turbidites in northwestern Sichuan, China: Implications for provenance and interpretation of the tectonic setting , 1994 .
[87] I. Mcdougall,et al. Noble gases in mafic phenocrysts and xenoliths from New Zealand , 1994 .
[88] R. Goldstein,et al. Systematics of fluid inclusions in diagenetic minerals , 1994 .
[89] Yong‐Fei Zheng. “Calculation of oxygen isotope fractionation in anhydrous silicate minerals.” Geochimica et Cosmochimica Acta , 1993 .
[90] J. Ramsay,et al. Eocene age of eclogite metamorphism in Pakistan Himalaya: implications for India-Eurasia collision , 1993 .
[91] M. Sasada. Analysis of fluid inclusion gases from geothermal system, using a rapid-scanning quadrupole mass spectrometer , 1992 .
[92] L. Colangeli,et al. Raman and Infrared Spectra of Polycyclic Aromatic Hydrocarbon Molecules of Possible Astrophysical Interest , 1992 .
[93] F. Stuart,et al. Helium/heat ratios and deposition temperatures of sulphides from the ocean floor , 1992, Nature.
[94] A. Cohen,et al. Isotopic relationships of volatile and lithophile trace elements in continental ultramafic xenoliths , 1992 .
[95] François Robert,et al. High-angle reverse faults, fluid-pressure cycling, and mesothermal gold-quartz deposits , 1988 .
[96] S. Sheppard. Characterization and isotopic variations in natural waters , 1986 .
[97] J. Andrews. The isotopic composition of radiogenic helium and its use to study groundwater movement in confined aquifers , 1985 .
[98] C. Ramboz,et al. Fluid immiscibility in natural processes: Use and misuse of fluid inclusion data: II. Interpretation of fluid inclusion data in terms of immiscibility , 1982 .
[99] J. Ferry. Petrology of graphitic sulfide-rich schists from South-central Maine; an example of desulfidation during prograde regional metamorphism , 1981 .