New understandings of Ni–Mo mineralization in early Cambrian black shales of South China: Constraints from variations in organic matter in metallic and non-metallic intervals
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[1] J. Mao,et al. Seawater contribution to polymetallic Ni–Mo–PGE–Au mineralization in Early Cambrian black shales of South China: Evidence from Mo isotope, PGE, trace element, and REE geochemistry , 2013 .
[2] S. Yao,et al. Organic clots and their differential accumulation of Ni and Mo within early Cambrian black-shale-hosted polymetallic Ni–Mo deposits, Zunyi, South China , 2013 .
[3] M. Böttcher,et al. Mo isotope and trace element patterns of Lower Cambrian black shales in South China: Multi-proxy constraints on the paleoenvironment , 2012 .
[4] F. Pirajno. Hydrothermal Mineral Deposits: Principles and Fundamental Concepts for the Exploration Geologist , 2012 .
[5] Mao Jingwen,et al. Re-Os Age of Polymetallic Ni-Mo-PGE-Au Mineralization in Early Cambrian Black Shales of South China—A Reassessment , 2011 .
[6] Jinghong Yang,et al. Early Cambrian ocean anoxia in South China , 2009, Nature.
[7] A. Bekker,et al. Seafloor-hydrothermal Si-Fe-Mn exhalites in the Pecos greenstone belt, New Mexico, and the redox state of ca. 1720 Ma deep seawater , 2009 .
[8] J. Kramers,et al. Hydrogen sulphide release to surface waters at the Precambrian/Cambrian boundary , 2008, Nature.
[9] B. Orberger,et al. Multiple Sources of Metals of Mineralization in Lower Cambrian Black Shales of South China: Evidence from Geochemical and Petrographic Study , 2008 .
[10] J. Pašava,et al. Organic geochemistry and petrology of barren and Mo-Ni-PGE mineralized marine black shales of the Lower Cambrian Niutitang Formation (South China) , 2007 .
[11] Jinghong Yang,et al. Extreme enrichment of polymetallic Ni–Mo–PGE–Au in Lower Cambrian black shales of South China: An Os isotope and PGE geochemical investigation , 2007 .
[12] D. Ma,et al. Highly metalliferous carbonaceous shale and Early Cambrian seawater , 2007 .
[13] B. Orberger,et al. Biogenic origin of intergrown Mo-sulphide- and carbonaceous matter in Lower Cambrian black shales (Zunyi Formation, southern China) , 2007 .
[14] J. Grotzinger,et al. Evidence for anoxia at the Ediacaran–Cambrian boundary: the record of redox-sensitive trace elements and rare earth elements in Oman , 2007, Journal of the Geological Society.
[15] Jinghong Yang,et al. Trace- and rare-earth element geochemistry and Pb–Pb dating of black shales and intercalated Ni–Mo–PGE–Au sulfide ores in Lower Cambrian strata, Yangtze Platform, South China , 2006 .
[16] J. B. Maynard,et al. Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems , 2004 .
[17] Jinghong Yang,et al. Re-Os isotopes and PGE geochemistry of black shales and intercalated Ni-Mo polymetallic sulfide bed from the Lower Cambrian Niutitang Formation, South China , 2003 .
[18] D. Ma,et al. Re-Os Dating of Polymetallic Ni-Mo-PGE-Au Mineralization in Lower Cambrian Black Shales of South China and Its Geologic Significance , 2003 .
[19] Yoshio Watanabe,et al. Oceanic anoxia at the Precambrian-Cambrian boundary , 2001 .
[20] J. Penner‐Hahn,et al. A C/MoS2 mixed-layer phase (MoSC) occurring in metalliferous black shales from southern China, and new data on jordisite , 2001 .
[21] Yuan-long Zhao,et al. Submarine-hydrothermal exhalative ore layers in black shales from South China and associated fossils — insights into a Lower Cambrian facies and bio-evolution , 2001 .
[22] J. Murowchick,et al. Sedimentary exhalative nickel-molybdenum ores in South China , 1999 .
[23] M. Schidlowski,et al. Geochemical changes across the Proterozoic–Cambrian transition in the Durmala phosphorite mine section, Mussoorie Hills, Garhwal Himalaya, India , 1997 .
[24] G. Zhenmin,et al. Silicalites of hydrothermal origin in the Lower Cambrian black rock series of South China , 1996 .
[25] K. H. Wedepohl,et al. The Composition of the Continental Crust , 1995 .
[26] K. Shelton,et al. Cyclic variations of sulfur isotopes in Cambrian stratabound Ni-Mo- ( PGE-Au) ores of southern China , 1994 .
[27] M. Glascock,et al. Gold and platinum in shales with evidence against extraterrestrial sources of metals , 1992 .
[28] M. Brasier. Background to the Cambrian Explosion , 1992, Journal of the Geological Society.
[29] C. Nansheng,et al. Ni-Mo-PGE-Au-rich ores in Chinese black shales and speculations on possible analogues in the United States , 1991 .
[30] C. Nansheng,et al. Lower Cambrian black rock series and associated stratiform deposits in Southern China , 1990 .
[31] K. Turekian,et al. Distribution of the Elements in Some Major Units of the Earth's Crust , 1961 .
[32] Bi Kun. Geochemical Characteristics of Selenium-rich Strata and Weathered Soil from Kaiyang County,Guizhou Province , 2012 .
[33] K. Zhao,et al. Highly metalliferous carbonaceous shale and Early Cambrian seawater: COMMENT and REPLY COMMENT , 2007 .
[34] Lin Li,et al. The characteristics of organic matter and its mineralization in the Jinding lead-zinc deposit,Yunnan,China , 2006 .
[35] Jiang Yong-hong,et al. A study of the fluid environment of silicalite of transitional Precambrian-Cambrian age in Hunan and Guizhou provinces , 2005 .
[36] Xia Fei,et al. STUDY ON NICKEL AND MOLYBDENUM MINERALS IN Ni-Mo SULFIDE LAYER OF THE LOWER CAMBRIAN BLACK ROCK SERIES,NORTHWESTERN HUNAN , 2005 .
[37] Bao Miao. A Study on Characteristics of the Hydrothermal Vent and Relating Biota at the Cambrian Bottom in Songlin, Zunyi County, Guizhou Province , 2005 .
[38] J. Pašava,et al. Diverse connections between ores and organic matter , 2004 .
[39] Mao Jingwen. Geology, Geochemistry, and Re-Os Isotopic Dating of the Huangjiawan Ni-Mo-PGE Deposit, Zunyi, Guizhou Province ——with a Discussion of the Polymetallic Mineralization of Basal Cambrian Black Shales in South China , 2001 .
[40] M. Zeng. Geological Feature of the Huangjiawan Ni-Mo Deposit in Zunyi of Guizhou and its Prospect for Development , 1998 .
[41] J. Morgan,et al. Rhenium and osmium isotopes in black shales and Ni-Mo-PGE-rich sulfide layers, Yukon Territory, Canada, and Hunan and Guizhou provinces, China , 1994 .