2013-08-15
一.导师简介
侯增谦,研究员,1961年 6 月生,河北省人,博士生导师,国家杰出青年基金获得者,国家973项目首席科学家,2008年受聘江西省“井冈学者” 东华理工大学特聘教授。
1982年毕业于河北地质学院地质系,1985年.1988年在中国地质大学获硕士学位和博士学位。1993-1994在日本地质调查所任客座研究员。目前兼任中国矿物岩石地球化学学会理事.中国大洋钻探科学委员会委员.《中国科学》特邀编委.《矿床地质》副主编.《地质论评》.《中国地质》.《岩石矿物学杂志》.《现代地质》编委等职。1992年曾获中国地质学会“金锤奖”,1996年入选人事部等7部委“跨世纪人才工程”,2006 获第三届黄汲清青年科技奖。
20多年来,他和合作者发表论文228篇,SCI收录73篇(第一作者28篇);在国际学术期刊主编英文专集3部,出版专著7部;SCI论文引用778次,他引566次,CSCD论文引用1626次,他引1136次;曾获第六届中国青年科学家提名奖和第三届黄汲清青年科技奖等奖项。
二.公开发表的学术论文
1. Hou Z.-Q., Cook N., 2009, Metallogenesis of the Tibetan Collisional Orogen: A review and introduction to the special issue. Ore Geology Reviews,36: 1-28 (SCI).
2. Hou Z.-Q., Qu X.-M., Rui, Z.-Y., Meng, X.-J., Gao Y.-F., 2009, The Gangdese Miocene porphyry copper belt generated during post-collisional extension in the Tibetan orogen. Ore Geology Reviews, dx.doi.org/10.1016/j.oregeorev.2008.10.007 (SCI).
3. Hou Z.-Q., Tian S.-H., Xie Y.-L., et al., 2009, The Himalayan Mianning-Dechang REE belt associated with carbonatite-alkalic complex in the eastern Indo-Asian collision zone, SW China. Ore Geology Reviews, dx.doi.org/10.1016/j.oregeorev.2008.12.001 (SCI).
4. Hou Z.-Q., Zaw Khin, Rona Peter, Li Y.-Q., Qu X.-M., Song S.-H., Peng L.-G., Huang J.-J., 2008, Geology, fluid inclusions and oxygen isotope geochemistry of the Baiyinchang Pipe-Style Volcanic Hosted Massive Sulfide Cu Deposit in Gansu Province, Northwestern China: evidence for sub-seafloor Replacement and Fluid Mixing. Economic Geology, 103: 269-292 (SCI).
5. 侯增谦,宋玉财,李政,王召林,杨志明,杨竹森,刘英超,田世洪,何龙清,陈开旭,2008. 青藏高原碰撞造山带Pb-Zn-Ag矿床新类型:成矿基本特征与构造控矿模型. 矿床地质,27:123-144.
6. 侯增谦,田世洪,谢玉玲,袁忠信,杨竹森,杨志明, 尹淑苹, 费红彩,邹天人,李小渝,2008. 川西冕宁-德昌喜马拉雅期稀土成矿带:矿床地质特征与区域成矿模型. 矿床地质,27:145-176.
7. 侯增谦,王二七,2008. 印度-亚洲大陆碰撞成矿作用主要研究进展. 地球学报,29:275-292.
8. Hou Z-Q, Xie Y-L, et al., 2007, Yulong deposit, East Tibet: A high-sulfidation Cu-Au porphyry Cu deposit in the eastern Indo-Asian collision zone. International Geology Reviews,49: 235-28 (SCI).
9. Hou Z-Q, Pan Guitang, Mo Xuanxue, Xu Qiang, Hu Yunzhong,Li Xingzhen,2007, The Sanjiang Tethyan metallogenesis in S.W. China: tectonic setting, metallogenic epoch and deposit type. Ore Geology Reviews, 31 (1-4): 48-87 (SCI).
10. Hou Z.-Q., Yang Z-S., et al., 2007, Geo-fluid mapping in the Tongling: Implications for the Paleozoic Submarine Hydrothermal System in the Middle-Lower Yangtze Metallogenic Belt, East China. Acta Geologica Sinica, 81(5): 833-860 (SCI).
11. Hou Z.-Q., 2007. Metallogenesis of the Tibetan collisional orogen, Jour. China Univ. Geosci., 18(S1): 243-244. (SCI) Hou Z.-Q., Tian Shihong, Yuan Zhongxin, Xie Yuling, 2006, The Himalayan collision zone carbonatites in Western Sichuan, SW China: petrogenesis, mantle source and tectonic implication. Earth Planet. Sci. Lett., 244: 234-250 (SCI).
12. Hou Z-Q., Zeng P-S., Gao Y.-F., 2006, The Himalayan Cu-Mo-Au mineralization in the eastern Indo-Asian collision zone: constraints from Re-Os dating of molybdenite. Minerlium Deposita, 41: 33-45 (SCI).
13. Hou Z.-Q., Chen Wen, Lu Jiren, et al, 2006, Eruption at ~259 Ma of the continental flood basalts in the Emeishan large igneous province, SW China: Evidence from Laser Microprobe 40Ar/39Ar dating. Acta Geologica Sinica,80: 804-808 (SCI).
14. Hou Z-Q., Lu Jiren, Lin Shengzhong, 2006, Heterogeneity of a Plume Axis: bulk-rock geochemical evidence from picrites and basalts in the Emei Large Igneous Province, SW China. International Geology Review,48: 1087-1112. (SCI).
三.公开出版专著与教材
1. 侯增谦.韩发.夏林圻.张绮玲等,2003,现代与古代海底热水成矿作用. 地质出版社:北京, 423p
2. 侯增谦.杨岳清.王海平.曲晓明.黄典豪等,2003,西南三江义敦岛弧造山过程与成矿系统. 地质出版社:北京, 345p
3. 侯增谦.侯立纬.叶庆同.刘福禄.唐国光,1995, 三江义敦岛弧火山作用与火山成因块状硫化物矿床. 地震出版社:北京
4. 潘桂棠.徐强.侯增谦等, 2003, 中国西南特提斯造山带形成演化与成矿系统. 地质出版社:北京 430p.
5. 段锦荪.侯增谦等,2000, 滇西昌宁-孟连多金属成矿带地质. 地质出版社:北京,
6. 莫宣学.路风香.沈上越.朱勤文.侯增谦.杨开辉等, 1993,三江特提斯火山作用与成矿. 地质出版社:北京
7. Ancient and Modern Volcanogenic Massive Sulfide Deposits. Eds. by Peter Rona (美) and Zengqian Hou, In Exploration and Mining Geology , 1999,Vol.8,No.3/4
8. Mineral Deposits in South China. Eds. by Khin Zaw (澳), and Stephen Peters(美), N. Cook, and Zengqian Hou, In Ore Geology Reviews , 2006.
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