

胡瑞忠



胡瑞忠

中文名胡瑞忠

工作单位中国科学院地球化学研究所

民族汉

担任职务矿床地球化学国家重点实验室主任

教育背景成都地质学院

国籍中国

目录导航

人物经历

1978年3月-1988年3月，成都地质学院学习，获学士、硕士、博士学位。

1988年4月-1988年12月，成都地质学院，讲师。

1989年1月-1991年7月，中国科学院地球化学研究所，博士后。

1991年7月-至今，中国科学院地球化学研究所，副研究员、研究员。

1992年6月-1992年12月，新西兰地质与核科学研究所(IGNS, New Zealand)，访问研究。

1995年11月-1996年6月，英国曼彻斯特大学(University of Manchester)，访问研究。

2001年12月-2002年5月，美国加州理工学院(California Institute of Technology)，访问研究。

2003年2月-2003年5月，2005年6—2005年9月，2008年5月—2008年8月，香港大学访问研究。^[3]

研究方向

矿床地球化学和同位素地球化学研究。

负责的主要项目有：

（1）大规模成矿作用及大型矿集区预测（国家973项目，1999.10-2004.9，首席科学家）

（2）热液矿床矿化剂地球化学（国家杰出青年基金项目，1999.1-2002.12，负责人）

（3）华南白垩-第三纪岩石圈伸展与区域铀成矿关系研究（国家自然科学基金重点项目，2007.1-2010.12，负责人）

（4）华南陆块陆内成矿作用：背景与过程（国家973项目，2007.8-2011.12，首席科学家）

（5）扬子地块西南缘中生代大面积低温成矿年代学和动力学（国家自然科学基金重点项目，2013.1-2017.12，负责人）

（6）华南大规模低温成矿作用（国家973项目，2014.1-2018.8，首席科学家）^[3]

主要成就

科研成果

胡瑞忠在金、铀、铜、铅、锌、锗等矿床的地球化学和同位素地球化学等领域，取得了一系列重要研究成果，为发展我国的地球科学事业做出了重要贡献。

取得的主要成果包括：

（1）初步揭示了华南铀矿床绝大多数都是在白垩— 第三纪地壳拉张期形成的热液铀矿床的内在机制；

（2）为稀有气体同位素应用于固体矿床的成因示踪，提供了较多成功的研究实例；

（3）确定了滇黔桂地区卡林型金矿成矿热液可能的演化途径和深部作用过程对哀牢山金矿带金成矿的制约关系，提出了铜矿新类型—富碱斑岩铜矿的成矿模式；

（4）确定了分散元素Ge超常富集形成超大型锗矿床的机制；

（5）作为国家“973”项目首席科学家领导的 “大规模成矿作用及大型矿集区预测”研究，在大面积低温成矿域的形成机制、大规模成矿的地球动力学背景、大规模成矿的物质和能量传输等领域取得了重要研究成果。

主要论著

发表SCI论文200余篇，出版专（编）著9部。代表性论著有：

[1]Blattner P, Hu RZ, et al., Temperatures and isotopic evolution of silicic magmas, Taupo Volcanic Zone and Coromandel, New Zealand,N. Z. J. Geol. Geophys., 1996, 39: 353-362.

[2]Hu RZ, Burnard PG, et al., Helium and argon isotope systematics in fluid inclusions of Machangqing copper deposit in west Yunnan province, China, Chemical Geology, 1998, 146: 55-63.

[3]Burnard PG,Hu RZ, et al., Mantle, crustal and atomspheric noble gases in Ailaoshan gold deposits, Yunnan province, China, Geochim. Cosmochim. Acta, 1999, 63: 1595-1604.

[4]Hu RZ, Su WC, et al., Geology and geochemistry of Carlin-type gold deposits in China, Mineralium Deposita, 2002, 37: 378-392.

[5]Bi XW, Cornell DH, Hu RZ, REE composition of primary and altered feldspar from the mineralized alteration zone of alkali-rich intrusive rocks, western Yunnan province, China, Ore Geology Reviews, 2002,19: 69-78.

[6]Fang WX, Hu RZ, et al., Influence of black shales on soils and edible plants in the Ankang area, Shanxi Province, China, Environmental Geochemistry and Health, 2002, 24: 35-46.

[7]Peng JT, Hu RZ, et al., Samarium-Neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): The potential of calcite as a geochronometer, Chemical Geology, 2003, 200 : 129-136.

[8]Hu RZ, Burnard PG, et al., Helium and argon isotope geochemistry of alkaline intrusion-associated gold and copper deposits along the Red River-Jinshajiang fault belt, SW China, Chemical Geology, 2004, 203:305-317.

[9]Lee XQ, Hu RZ, et al., Ontogenetic trace element distribution in brachiopod shells: an indicator of original seawater chemistry, Chemical Geology, 2004, 209: 49-65.

[10]Bi XW, Hu RZ, et al., The alkaline porphyry associated Yao'an gold deposit, Yunnan, China: rare earth element and stable isotope evidence for magmatic-hydrothermal ore formation, Mineralium Deposita, 2004,39:21-30.

[11]Jia DC, Hu RZ, et al., Collision belt between the Kyanka block and the North China block in Yanbian region, Northeast China, Journal of Asian Earth Sciences,2004, 23: 211-219.

[12]Zhao JH, Hu RZ, et al., Geochemistry, petrogenesis, and tectonic significance of Mesozoic mafic dikes, Fujian province, Southeastern China, International Geology Review, 2004, 46:542-557.

[13]Zhong H,Hu RZ, et al., Review of the Link between the Hongges Layered Intrusion and Emeishan Flood Basalts, Southwest China: Internationgal Geology Review, 2005, 47, 971-985.

[14]Liu S, Zou HB, Hu RZ, et al., Mesozoic mafic dikes from the Shandong Peninsula, North China Craton: Petrogenesis and tectonic implications, Geochemical Journal, 2006, 40: 181-195.

[15]Li ZL, Hu RZ, et al., Helium isotope geochemistry of ore-forming fluids from Furong tin orefield in Hunan Province, China, Resource Geology, 2006, 56: 9-15.

[16]Xie GQ, Hu RZ, et al., K-Ar dating, geochemical, and Sr-Nd-Pb isotopic systematics of late Mesozoic mafic dikes, southern Jiangxi Province, Southeast China: Petrogenesis and tectonic implications, International Geology Review, 2006, 48: 1023-1051.

[17]Peng JT, Zhou MF, Hu RZ, et al., Precise molybdenite Re-Os and mica Ar-Ar dating of the Mesozoic Yaogangxian tungsten deposit, central Nanling district, South China, Mineralium Deposita, 2006, 41: 661-669.

[18]Zhao JH, Hu RZ, et al., Elemental and Sr-Nd-Pb isotopic geochemistry of Mesozoic mafic intrusions in southern Fujian province, SE China: implications for lithospheric mantle evolution, Geological Magazine, 2007, 144: 937-952.

[19]Li ZL, Hu RZ, et al., He, Pb and S isotopic constraints on the relationship between the A-type Qitianling granite and the Furong tin deposit, Hunan Province, China, Lithos, 2007, 97: 161-173.

[20]Qi HW, Hu RZ, et al., Concentration and distribution of trace elements in lignite from the Shengli Coalfield, Inner Mongolia, China: Implications on origin of the associated Wulantuga Germanium Deposit, International Journal of Caol Geology, 2007, 71: 129-152.

[21]Qi HW, Hu RZ, et al., REE Geochemistry of the Cretaceous lignite from Wulantuga Germanium Deposit, Inner Mongolia, Northeastern China, International Journal of Caol Geology, 2007, 71: 329-344.

[22]Tao Y, Li CS, Hu RZ, et al., Petrogenesis of the Pt-Pd mineralized Jinbaoshan ultramafic intrusion in the Permian Emeishan Large Igneous Province, SW China, Contributions to Mineralogy and Petrology, 2007, 153: 321-337.

[23]Hu RZ, Bi XW, et al., Uranium metallogenesis in South China and its relationship to crustal extension during the Cretaceous to Tertiary,Economic Geology, 2008, 103：583-598.

[24]Liu S, Hu RZ, et al., U-Pb zircon age, geochemical and Sr-Nd-Pb-Hf isotopic constraints on age and origin of alkaline intrusions and associated mafic dikes from Sulu orogenic belt, Eastern China, Lithos, 2008, 106: 365-379.

[25]Hu XY, Bi XW, Hu RZ, et al., Experimental study on tin partition between granitic silicate melt and coexisting aqueous fluid, Geochemical Journal, 2008, 42: 141-150.

[26]Liu S, Hu RZ, et al., Zircon U-Pb geochronology and major, trace elemental and Sr-Nd-Pb isotopic geochemistry of mafic dykes in western Shandong Province, east China: Constrains on their petrogenesis and geodynamic significance, Chemical Geology, 2008, 255: 329-345.

[27]Liu S, Hu RZ, et al., K-Ar ages and geochemical plus Sr-Nd isotopic compositions of adakitic volcanic rocks, western Shandong Province, eastern China: Foundering of the lower continental crust, International Geology Review, 2008, 50: 763-779.

[28]Liu S, Hu RZ, et al., Cenozoic high Sr/Y volcanic rocks in the Qiangtang terrane, northern Tibet: geochemical and isotopic evidence for the origin of delaminated lower continental melts, Geological Magazine, 2008, 145: 463-474.

[29]Yuan SD, Peng JT, Hu RZ, et al., A precise U-Pb age on cassiterite from the Xianghualing tin-polymetallic deposit (Hunan, South China), Mineralium Deposita, 2008, 43: 375-382.

[30]Hu RZ, Burnard PG, et al., Mantle-derived gaseous components in ore-forming fluids of the Xiangshan uranium deposit, Jiangxi province, China: Evidence from He, Ar and C isotopes, Chemical Geology, 2009, 266: 86-95.

[31]Hu RZ, Qi HW, et al., Geological and geochemical constraints on the origin of the giant Lincang coal seam-hosted germanium deposit, Yunnan, SW China: A review, Ore Geology Reviews, 2009, doi:10.1016/j.oregeorev.2009.02.007.

[32]Liu S, Hu RZ, et al., Zircon U-Pb age, geochemistry and Sr-Nd-Pb isotopic compositions of adakitic volcanic rocks from Jiaodong, Shandong Province, Eastern China: Constraints on petrogenesis and implications, Journal of Asian Earth Sciences, 2009, 35: 445-458.

[33]Zhong H, Zhu WG, Hu RZ, et al., Zircon U-Pb age and Sr-Nd-Hf isotope geochemistry of the Panzhihua A-type syenitic intrusion in the Emeishan large igneous province, southwest China and implications for growth of juvenile crust, Lithos, 2009, 110: 109-128.

[34]Cao JJ, Hu RZ, et al., TEM observation of geogas-carried particles from the Changkeng concealed gold deposit, Guangdong Province, South China, Journal of Geochemical Exploration, 2009, 101: 247-253.

[35]Bi XW, Hu RZ, et al., Crystallisation conditions (T, P, fO(2)) from mineral chemistry of Cu- and Au-mineralised alkaline intrusions in the Red River-Jinshajiang alkaline igneous belt, western Yunnan Province, China, Mineralogy and Petrology, 2009, 96: 43-58.

[36]Su WC, Hu RZ, et al., Calcite Sm-Nd isochron age of the Shuiyindong Carlin-type gold deposit, Guizhou, China, Chemical Geology, 2009, 258: 269-274.[3]

[37]胡瑞忠、毛景文、华仁民、范蔚茗, 华南陆块陆内成矿作用，科学出版社, 2015, 1-903, 北京.

[38]Hu RZ, Liu JM, Zhai MG. Mineral Resources Science in China, A Roadmap to 2050, Science Press, Springer, 2010, 1-94.

[39]Hu RZ, Bi XW, Zhou MF, Peng JT, Su WC, Liu S, Qi HW. Uranium metallogenesis in South China and its relationship to crustal extension during the Cretaceous to Tertiary. Economic Geology, 2008, 103: 583-598.

[40]Hu RZ, Burnard PG, Bi XW, Zhou MF, Peng JT, Su WC, Zhao JH. Mantle-derived gaseous components in ore-forming fluids of the Xiangshan uranium deposit, Jiangxi province, China: Evidence from He, Ar and C isotopes, Chemical Geology, 2009, 266: 86-95.

[41]Hu RZ, Bi XW, Jiang GH, Chen HW, Peng JT, Qi YQ, Wu LY, Wei WF. Mantle-derived noble gases in ore-forming fluids of the granite-related Yaogangxian tungsten deposit, Southeastern China. Mineralium Deposita, 2012, 47: 623-632.

[42]Hu RZ, Zhou MF. Multiple Mesozoic mineralization events in South China. Mineralium Deposita, 2012, 47: 579-588.

[43]Zhu JJ, Hu RZ, Righards JP, Bi XW, Zhong H. Genesis and magmatic-hydrothermal evolution of the Yangla skarn Cu deposit, Southwest China. Economic Geology, 2015, 110: 631-652.

[44]Hu RZ, Fu SL, Huang Y, Zhou MF, Fu SH, Zhao CH, Wang YJ, Bi XW, Xiao JF. The giant South China Mesozoic low-temperature metallogenic domain: Review and a new geodynamic model. Journal of Asian Earth Sciences, 2017, 137: 9–34.

[45]Pi QH, Hu RZ, Xiong B, Li QL, Zhong RC. In situ SIMS U-Pb dating of hydrothermal rutile: reliable age for the Zhesang Carlin-type gold deposit in the golden triangle region, SW China. Mineralium Deposita, 2017, 52: 1179-1190.

[46]Wu LY, Hu RZ, Li XF, Stuart FM, Jiang GH, Qi YQ, Zhu JJ. Mantle volatiles and heat contributions in high sulfidation epithermal deposit from the Zijinshan Cu-Au-Mo-Ag orefield, Fujian Province, China: Evidence from He and Ar isotopes. Chemical Geology, 2018, 480: 58-65^[3]