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《Acta Petrologica Sinica》 2008-03
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Petrogenesis and metallogenesis of the Beiya gold- polymetallic ore district,northwestern Yunnan province,China: Responses to the Indo-Asian collisional processes

XUE ChuanDong~(1,2) HOU ZengQian~2 LIU Xing~1 YANG ZhiMing~2 LIU YongQiang~1 HAO BaiWu 1.Department of Earth Sciences,Kunming University of Science and Technology,Kunming 650093,Yunnan,China 2.Institute of Geology,Chinese Academy of Geological Science,Beijing 100037,China  
Beiya gold-polymetallic ore district found in northeastern Yunnan province in the last few years,located in the middle- southern section of the eastern Xizang-Jinsha River - Ailao Mountain alkali-rich porphyry metallogenetic belt,is one of the typical gold-polymetallic metallogenesis system related to alkali-rich intrusion during the Himalayan epoch.Based on the previous researches and the extensive field investigations from the recent scientific programs,this article systematically studies the petrogenesis, metallogenesis evolving sequence in the ore district and their responses to the Indo-Asian collisional processes.The main intrusion rock types including quartz-albite porphyry,quartz-K-feldspar porphyry and biotite-K-feldspar porphyry with adakitic magma affinity,which intruded during the period of 65 to 59 Ma,36 to 32 Ma,26 to 24 Ma and 3.8 to 3.6 Ma respectively.The magmas of ore-bearing alkali-rich porphyries were derived from mixed melting of the crust-mantle transitional layer in eastern margins of the Tibet plateau,and genetically related to the asthemosphere eastern-extruding and the large-scale strike-slip faulting due to the Himalayanian Indo-Asian collisional systems.The duration of the first episode and the second episode are consisted with the two concentrative petrogenesis episodes approximately.Within the ore district,three types and seven subclasses of gold-polymetallic deposits have been recognized, there are (Ⅰ) porphyry copper-gold-polymetallic deposits related to the first and second stage of alkali-rich porphyry intrusion,including skarn-type gold-polymetallic deposits (including magma-type ),porphyry-type copper-gold deposits and hydrothermal-type gold- polymetallic deposits,(Ⅱ)porphyry-related hydrothermal-type gold-polymetallic deposits due to the third stage of alkali-rich porphyry intrusion,including cryptoexplosive breccia-type gold-ferrous-lead- zinc-polymetallic deposits and hydrothermal superimposed-type gold-polymetallic deposits,and (Ⅲ) weathered-sedimentary-type deposits associated with the fluvial and lacustrine sedimentary rocks formed by the surface weathering and the laterization,including red clay-type gold deposits and palaeoplacer-type gold deposits.The Ⅰ-and Ⅱ-type deposits were controlled directly by the alkali-rich porphyry intrusion and NE-NNE-trending strike-slip faulting,and occur in the porphyry intrusions,the cryptoexplosive breccia pipes,the porphyry contacts and the porphyry outside contacts of the fractured zone and the intensive joint zone within middle Triassic limestone of Beiya Formation.The earlier deposits usually were overprinted by the later epithermal mineralization system associated with late magmatism,which formed either isolated,but spatially coexisted a high-grade giant deposit,and all provided the material sources for the palaeoplacer-type deposits.Correspondingly,ore- forming mineralization also changed from Cu-Au-(Mo) associations,Fe-Cu-Au-Pb-Zn associations to Au-Pb-Zn-Ag associations,the mineralization resources and fluid resources both come from the alkali-rich porphyries magmatism,and construct a porphyry- hydrothermal metallogenic system,the wall rocks only provide a space for the metal deposition.The secondary enrichment and supergenetic mineralization began at the time of the primary gold deposits occurrence,and brought up various weathered-sedimentary- type deposits.Among them,the palaeo red clay-type gold deposits formed during the period from Eocene to Oligocene,the palaeoplacer gold deposits formed during the period from 23 to 5Ma,and the modem red clay-type (including eluvium-type) gold deposits continued all along.Comparing to the regional evolution sequences,it is explained that the Beiya gold-polymetallic deposits be controlled by the evolution of the Indo-Asian collisional orogen and tectonomagmatism under the collision belt,which implies the same dynamic setting of paroxysmal mineralization of porphyry-type deposits to the eastern Xizang-Jinsha River-Ailao Mountain porphyry metallogenetic belt,displayed the long-distance effects in the structural transform zone of the main collisional orogenic setting since the Palaeocene.Episodically stress relaxation during tectonically transforming from transpressional(55~40 Ma) to transtensional(24~17 Ma)regimes probably caused multiple magmatic intrusions,which most likely result in the protraction of the hydrothermal system and superimprosed mineralization in the eastern Indo-Asian continental collision zone,and the duration from 36 to 32Ma is the main mineralization period of the porphyry- hydrothermal metallogenic system.There are great gold-polymetallic prospective reserves within the deep areas of ore district and surrounding regions.It is possible that the Yanyuan-Lijiang fault control a comparatively independent porphyry metallogenetic belt with close relationship to the Xizang-Jinsha River-Ailao Mountain porphyry metallogenetic belt.
【Fund】: 国家基础研究计划“印度-亚洲大陆主碰撞带成矿作用”973项目综合课题(编号:2002CB4126);; 国家自然科学基金项目(编号:40772067);; 云南省自然科学基金项目(编号:2006D020M);; 云南省省院省校科技合作项目(编号:YK98008-2)资助
【CateGory Index】: P618.2
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【References】
Chinese Journal Full-text Database 4 Hits
1 YANG ZhiMing and HOU ZengQian (Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China);Porphyry Cu deposits in collisional orogen setting:A preliminary genetic model[J];Mineral Deposits;2009-05
2 DENG Jun1,YANG LiQiang1,GE LiangSheng2,3,YUAN ShiSong2,WANG QingFei1,ZHANG Jing1,GONG QingJie1 and WANG ChangMing11. State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China2. Gold Geological Institute of Chinese People's Armed Police Force,Langfang 065000,China 3. Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;Character and post-ore changes,modifications and preservation of Cenozoic alkali-rich porphyry gold metallogenic system in western Yunnan,China[J];Acta Petrologica Sinica;2010-06
3 XUE ChuanDong1,LUO ShaoYong1,SONG YuCai2,YANG ZhiMing2,HAN YanWei1,HUANG QinHui1,LI Jing1 and WEI AiYing11. Department of Earth Sciences,Kunming University of Science and Technology,Kunming 650093,China2. Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;Zircon SHRIMP U-Pb dating and its geological significance of Lujiacun quartz-monzonite porphyry in Shangri-la County,northwestern Yunnan Province,China[J];Acta Petrologica Sinica;2010-06
4 CHEN JianLin1,XU JiFeng1,WANG BaoDi1,2 and KANG ZhiQiang1,21. Key Laboratory of Isotope Geochronology and Geochemistry,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou510640,China2. Graduate School of Chinese Academy of Sciences,Beijing 100039,China;Geochemical comparison of Paleogene high-Mg potassic volcanic rocks in Sanjiang area and interior Tibetan Plateau:Compositional difference of the mantle sources[J];Acta Petrologica Sinica;2010-06
【Citations】
Chinese Journal Full-text Database 10 Hits
1 LIU Xian-fan,SONG Xiang-feng,LU Qiu-xia,TAO Zhuan,LONG Xun-rongCollege of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;Mantle Fluid's Action in the Processes of Petrogenesis of Alkalic Porphyry and Associated Mineralizations,Western Yunnan,China-Constraint of Geochronology and Isotope Geochemistry[J];Journal of Jilin University(Earth Science Edition);2006-04
2 WANG Yun sheng, WANG Shi tian (Chengdu University of Technology, China);THE GENETIC MECHANISM ANALYSIS OF THE NAPPES IN THE JIANCHUAN-HEQING REGION, YUNNAN[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;2000-02
3 HU Xiangzhao;HUANG Zhen(Department of Geology, Central South University of Technology, Changsha 410083)(China National Nonferrous Metal Industrial Corporation,General Bureau of Geology, Beijing, 100814);THE PETROLOGY AND PETROGENSIS OF THE YANGTZE PLATFROM WESTERN MARGINIS ALKALI-RICH GRANITE PORPHYTY[J];GEOTECTONICA ET METALLOGENIA;1997-02
4 LAI Jianqing; PENG Shenglin; WANG He; SHAO Yongjun(Department of Geology, Central South University of Technology, Changsha 410083);ON THE METALLOGENETIC MECHANISM OF THE ALKALI-RICH PORPHYRIES IN CENTRAL YUNNAN[J];GEOTECTONICA ET METALLOGENIA;1997-04
5 HOU Zeng-qian 1 ,ZHONG Da-lai 2 ,DENG Wan-ming 2(1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing100037,China;2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing100029,China);A tectonic model for porphyry copper-molybdenum-gold metallogenic belts on the eastern margin of the Qinghai-Tibet Plateau[J];Chinese Geology;2004-01
6 LIU Hongying XIA Bin ZHANG Yuquan (Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry,CAS,Guangzhou,Guangdong,510640);The SHRIMP U-Pb Age of Matouwan Diopside Granite Porphyry in Yunnan Province[J];Acta Geosicientia Sinica;2003-06
7 Zhong Dalai, Ding Lin, Ji Jianqing, Zhang Jinjiang, Liu Futian, Liu Jianhua, Yan Xiaowei (① Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029; ② Department of Geology, Peking University, Beijing 100871);COUPLING OF THE LITHOSPHERIC CONVERGENCE OF WEST CHINA AND DISPERSION OF EAST CHINA IN CENOZOIC: LINK WITH PALEOENVIRONMENTAL CHANGES[J];Quaternary Sciences;2001-04
8 WANG Qiang, XU Ji feng,ZHAO Zhen hua (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640,China);THE SUMMARY AND COMMENT ON RESEARCH ON A NEW KIND OF IGNEOUS ROCK—ADAKITE[J];Advance In Earth Sciences;2001-02
9 MO Xuan-xue,ZHAO Zhi-dan,DENG Jin-fu,DONG Guo-chen,ZHOU Su,GUO Tie-ying,ZHANG Shuang-quan,WANG Liang-liang(School of Earth Sciences and Mineral Resources, China University of Geosciences,Beijing 100083, China);RESPONSE OF VOLCANISM TO THE INDIA-ASIA COLLISION[J];Earth Science Frontiers;2003-03
10 LUO Zhao-hua~ 1 , MO Xuan-xue~ 1 , HOU Zeng-qian~ 2 , DENG Wan-ming~ 3 , WANG Jiang-hai~ 4 , ZHAO Zhi-dan~ 1 , YU Xue-hui~ 1 , LI Jian-ping~ 4 1.State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083,China 2.Institute of Mineral Resources, CAGS, Beijing 100037,China 3.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029,China 4.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640,China;An integrated model for the Cenozoic evolution of the Tibetan plateau:constraints from igneous rocks[J];Earth Science Frontiers;2006-04
【Co-references】
Chinese Journal Full-text Database 10 Hits
1 GAO Jian- guo1, XIA Ji- sheng1,CHENG Chang- yong2 (1.Kunming University of Science and Technology, Kunming 650093, China) ( 2.Kunming City Land Planning Bureau, Kunming 650093, China);GEOCHEMICAL FEATURES OF ALKALI-RICH PORPHYRY AND ANALYSIS OF AU (POLYMETALLIC)DEPOSITS IN WESTERN YUNNAN[J];GEOTECTONICA ET METALLOGENIA;2000-S1
2 MA De yun1,2, GAO Zhen min1, YANG Shi yu2 and HAN Run sheng1,2 (1. Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China; 2. Department of Earth Sciences, Kunming University of Science and Technology, Kunming 650093, China);NUMERICAL SIMULATION FOR TECTONIC STRESS FIELD OF THE BEIYA GOLD DEPOSIT[J];Geotectonica Et Metallogenia;2003-02
3 XIA Bin, LIN Qingcha and ZHANG Yuquan(Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese academy of Sciences, Guangzhou, GD 510640, China);ZIRCON SHRIMP DATING OF DIOPSIDE GRANITE IN AILAOSHAN-JINSHAJIANG ROCK BELT AND ITS GEOLOGICAL IMPLICATIONS——EXAMPLE FOR YUZHAOKUAI, MATOUWAN AND SHILICUN DIOPSIDE GRANITES[J];Geotectonica Et Metallogenia;2005-01
4 WAN Shaokai 1,2, XIA Bin1 and ZHANG Yuquan1 (1. CAS Key Laboratory of Marginal Sea Geology and Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Graduate School, Chinese Academy of Sciences, Beijing 100039, China);SHRIMP ZIRCON U-PB DATING OF LAOJUNSHAN SYENITE[J];Geotectonica Et Metallogenia;2005-04
5 WU Genyao(Laboratory of Lithosphere Tectonic Evolution,Institute of Geology,Academia Sinica,Beijing,100029);TERTIARY THRUSTING-NAPPE STRUCTURES IN NORTHWEST YUNNAN,CHINA[J];GEOTECTONICA ET METALLOGENIA;1994-04
6 HOU Zeng-qian 1 ,ZHONG Da-lai 2 ,DENG Wan-ming 2(1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing100037,China;2.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing100029,China);A tectonic model for porphyry copper-molybdenum-gold metallogenic belts on the eastern margin of the Qinghai-Tibet Plateau[J];Chinese Geology;2004-01
7 HOU Zeng-qian, MO Xuan-xue, YANG Zhi-ming, WANG An-jian, PAN Gui-tang, QU Xiao-ming, NIE Feng-jun (Institute of Geology, China Academy of Geological Sciences, Beijing 100037, China; China University of Geosciences, Beijing 100082, China; Chinese Academy of Geological Sciences, Beijing 100037, China; Chengdu Institute of Geology and Mineral Resources, Chengdu, China; Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China);Metallogeneses in the collisional orogen of the Qinghai-Tibet Plateau: Tectonic setting, tempo-spatial distribution and ore deposit types[J];Geology in China;2006-02
8 Zhang Yuquan; Xie Yingwen; Liang Huaying; Qiu Huaning; Li Xianhua (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)Sun-Lin Chung (Department of Geology, Taiwan University, Taipei 10770);PETROGENESIS SERIES AND THE ORE-BEARING PORPHYRIES OF THE YULONG COPPER ORE BELT IN EASTERN TIBET[J];Geochimica;1998-03
9 HUANG Xiao-long , XU Yi-gang, YANG Qi-jun and QIU Hua-ning(Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Geochemistry of late Eocene high-Mg ultrapotassic lavas from western Yunnan, China: Constraints on petrogenesis[J];Geochimica;2007-02
10 Zhai Yusheng Deng Jun Peng Runmin (Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing100083, China);RESEARCH CONTENTS AND METHODS FOR POST-ORE CHANGES, MODIFICATIONS AND PRESERVATION[J];;2000-04
【Secondary References】
Chinese Journal Full-text Database 10 Hits
1 Xue Chunji~1,Zhao Zhanfeng~1,Wu Ganguo~1,Dong Lianhui~2,Feng Jing~2,Zhang Zhaochong~1, Zhou Gang~3,Chi Guoxiang~4,Gao Jinggang~5 1.State Key Laboratory of Geological Processes and Mineral Resources;Faculty of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China 2.Xinjiang Bureau of Geology and Mineral Resource Exploration,(U|¨)r(u|¨)mqi 830000,China 3.Geological Team-4,Xinjiang Bureau of Geology and Mineral Resource Exploration,Aletai 836500,China 4.Department of Geology,University of Regina,Regina Saskatchewan S4S 0A2,Canada 5.Faculty of Earth Sciences and Mineral Resources,Chang'an University,Xi'an 710054,China;The multiperiodic superimposed porphyry copper mineralization in Central Asian Tectonic Region:A case study of geology,geochemistry and chronology of Halasu copper deposit,Southeastern Altai,China.[J];Earth Science Frontiers;2010-02
2 Leng Chengbiao~(1,2),Zhang Xingchun~1,Zhou Weide~3 1.State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guizhou 550002,China 2.Graduate University of the Chinese Academy of Sciences,Beijing 100049,China 3.Sichuan Institute of Metallurgical Geology and Exploration,Chengdu 610051,China;A primary study of the geological characteristics and the zircon U-Pb age of the Gangjiang porphyry copper-molybdenum deposit in Nimu,Tibet.[J];Earth Science Frontiers;2010-02
3 FU De-gui1,ZHOU Yun-man1,ZHANG Chang-qing2,CHEN Qing-guang3,QIN Xiu-ping1(1.Yunnan Gold & Mining Group Co.Ltd.,Kunming 650224;2.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;3.No 1 Geology Party,Yunan Bureau of and Exploration,Qujing 655000);Geological Characteristics of Lamprophyres and their Relations with Gold Mineralization of the Xiaoshuijing Gold Deposit in Central Yunnan Province[J];Geology and Exploration;2010-03
4 XU Qing-sheng1,GUO Jian1,LIU Yang1,HUANG Shu-feng2,LI Qiu-ping2,CHEN Yu-shui2(1.Institute of Mineral Resources Research,CMGB,Beijing 100025;2.No.2 Institute of Geology and Mineral Exploration,CMGB,Putian,Fujian 351111);Application of Short Wave Infrared Spectrum Mineral Analyzer (BJKF-1) to Alteration Mineral Mapping at Panan,Tibet[J];Geology and Exploration;2011-01
5 QU XiaoMing,JIANG JunHua,XIN HongBo and CHEN Hua(Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China);A study of two groups of adakite almost simulteneously formed in Gangdese collisional orogen,Tibet:Why does one group contain copper mineralization and the other not?[J];Mineral Deposits;2010-03
6 WU JianHui1,FENG ChengYou2,ZHANG DeQuan2,LI JinWen2 and SHE HongQuan2(1 Hubei Geosciences Professional College,Jingzhou 434000,Hubei,China; 2 Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China);Geology of porphyry and skarn type copper polymetallic deposits in southern margin of Qaidam Basin[J];Mineral Deposits;2010-05
7 LONG Han-sheng,JIN Zhong-guo,ZHANG Lun-wei,CHEN Da,LIU Kai-kun(Geological and Mineral Resource Exploration Institute of Guizhou Non-ferrous Metal and Nucleus Industry Geological Bureau,Guiyang,Guizhou 550005);Advancement of research on polymetallic deposit in lower Cambrian black rock series in Guizhou province[J];Mineral Resources and Geology;2010-05
8 WANG ZhiHua,GUO XiaoDong,GE LiangSheng,FAN JunJie and XU Tao(Gold Geological Institute of CAPF,Langfang 065000,Hebei,China);Diagenetic and metallogenic epoch and ore-forming dynamic setting of Machangqing copper-polymetallic deposit,Yunnan Province[J];Mineral Deposits;2011-01
9 LI WanLun(China Geological Library,Beijing 100083,China);Advances in study of shallow fertile magma chambers below porphyry copper deposits[J];Mineral Deposits;2011-01
10 CHENG WenBin1,GU XueXiang1,TANG JuXing2,WANG LiQiang1,LV PengRui1,ZHONG KangHui3,LIU XiaoJi1 and GAO YiMing21.State Key Laboratory of Geological Process and Mineral Reources,China University of Geosciences,Beijing 100083,China2.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China3.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;Lead isotope characteristics of ore sulfides from typical deposits in the Gangdese-Nyainqentanglha metallogenic belt:Implications for the zonation of ore-forming elements[J];Acta Petrologica Sinica;2010-11
【Secondary Citations】
Chinese Journal Full-text Database 10 Hits
1 Zheng Shuhui, Zhang Zhifei, Ni Baolin, Hou Fagao, Shen Minzi Department of Geology, Department of Chemistry;Hydrogen and Oxygen Isotopic Studies of Thermal Waters in Xizang[J];Acta Scicentiarum Naturalum Universitis Pekinesis;1982-01
2 ZHU Jie-shou, CAI Xue-lin, CAO Jia-min, YAN Zhong-qiong (State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, China);Structure of lithosphere and implications of geodynamics in China and adjacent land and sea regions[J];Journal of Chengdu University of Technology(Science & Technology Edition);2004-06
3 DU Letian (Beijing Uranium Geology Research Institute);H-A-C-O-N-S MANTLE ICHOR[J];Geotectonica Et Metallogenia;1988-01
4 CHEN Guoda (Changsha Institute of Geotectonics, Academia Sinica Institute of Diwa Metallogeny, Central-South University of Technology);HISTORISTIC-CAUSATIONIST GEOTECTONICS[J];Geotectonica Et Metallogenia;1992-01
5 HU Xiangzhao;HUANG Zhen(Department of Geology, Central South University of Technology, Changsha 410083)(China National Nonferrous Metal Industrial Corporation,General Bureau of Geology, Beijing, 100814);THE PETROLOGY AND PETROGENSIS OF THE YANGTZE PLATFROM WESTERN MARGINIS ALKALI-RICH GRANITE PORPHYTY[J];GEOTECTONICA ET METALLOGENIA;1997-02
6 XIE Rongju;PENG Shenglin(Dept. of Geology, Cenral South University of Technology, Changsha 410083);K_2O CONTENT, K-METASOMATISM OF ROCK AND METALLOGENESIS[J];GEOTECTONICA ET METALLOGENIA;1998-03
7 LIN Ge; FAN Weiming; GUO Feng; WANG Yuejun(Changsha Institute of Geotectonics, Academia Sinica, Changsha 410013);THE CRUST-MANTLE TRANSITION LAYER AND TECTONIC EVOLUTION[J];GEOTECTONICA ET METALLOGENIA;1998-S1
8 MA De yun1,2, GAO Zhen min1, YANG Shi yu2 and HAN Run sheng1,2 (1. Open Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China; 2. Department of Earth Sciences, Kunming University of Science and Technology, Kunming 650093, China);NUMERICAL SIMULATION FOR TECTONIC STRESS FIELD OF THE BEIYA GOLD DEPOSIT[J];Geotectonica Et Metallogenia;2003-02
9 WU Genyao(Laboratory of Lithosphere Tectonic Evolution,Institute of Geology,Academia Sinica,Beijing,100029);TERTIARY THRUSTING-NAPPE STRUCTURES IN NORTHWEST YUNNAN,CHINA[J];GEOTECTONICA ET METALLOGENIA;1994-04
10 LAI Jianqing;PENG Shenglin(Dept.of Geolegy, Central-South University of Technology, Changsha 410083);ON THE TECTONICS AND COPPER METALLOGENY OF THE PREPLATFORM IN CENTRAL YUNNAN AND ITS NEIBORING DISTRICT[J];GEOTECTONICA ET METALLOGENIA;1996-01
China Proceedings of conference Full-text Database 1 Hits
1 Zeng Pusheng Yang Weiguang Yu Xuehui(China University of Gevsciences, Beijing);Alkli Porphyry Zone and the Relationship between the Porphyry and Gold Metallization in the Western Yunnan[A];[C];1999
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