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《Geochimica》 2004-06
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Petrochemistry and SHRIMP U-Pb zircon age of the Chongjiang ore-bearing porphyry in the Gangdese porphyry copper belt

LIN Wu,ZHANG Yu-quan,LIANG Hua-yin g,XIE Ying-wen Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistr y and South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou510640,China Correspondence should be addressed to LIN Wu(E-mail:linwu_2001@163.com)Received January 12,2004;revised April 19,2004;accepted August 31,2004;published November,2004  
The Gangdese porphyry copper belt is a new discovered ore belt in South Tib et,China.A lot of small ore-bearing intrusions,such as Chongjiang,Qulong,Nanmu,Tinggong,Dongga and Lakange,have been found in this ore belt.The Chongjiang porp hyritic intrusion occurs in the midd le part of the Gangdese porphyry copper belt in southern Qinghai-Xizang Plateau.The Chongjiang porphyry hosts 107m illion tons of metallic copper at an average tenor ranging from 0.48%to 0.63%and about 1.27million tons of me tallic Mo,and 21tons of metallic Au.The Chongjiang porphyry could be divided into early,main and late sta ges.The early stage rock and the main stage rock are diorite and granodioritic porphyry and quartz-monzonitic porphyry,respectively,and belon g to the high-alkaline series.The main stage granodioritic porphyry and quartz-monzonitic porphyry display massive,porphyritic texture,comprising pl agioclase,K-feldspar,minor mica a nd quartz as phenocrysts.The late stage is granitic porphyry,locating between the high-alkaline series and the sh oshonitic series.SHRIMP zircon dating of quartz-monzonitic porphyry for the Chongjiang porphyry is(12.9±0.3)Ma.It represents the formation age o f the ore-bearing porphyry.Our SHRIM P zircon age is younger than the previous zircon age犤(15.60±0.52)Ma,(14.54±0.65)Ma 犦and the related Re-Os age犤(14.85±0.69)Ma,(14.04±0.16)Ma 犦.The Chongjiang ore-bearing porphyry has two different ranges of ages:12~13.8Ma and 14~15.6Ma.It is suggested that magmatic activity of the Chongjiang ore-bearing porphyry is multiperio d.The first stage is 14~15.6Ma in age,and the second stage is 12~13.8Ma.Based on our new age data,together with the previous work,it is concluded that the diagenetic and metallogenic epoch of the ore-bearing porphyries in t he Gangdese porphyry copper belt is 18Ma to 12Ma.Duration of magmatic activity of the ore-bearing porphyries is a bout 6Ma.
【Fund】: 国家重点基础研究发展规划项目(G1999043203);; 中国科学院知识创新工程重要方向项目(KZCX2-SW-117);; 中国科学院知识创新工程领域前沿项目(GIGCX-03-04);; 国家自然科学基金(40472049)
【CateGory Index】: P597.3
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7 CHEN Maohong1,2),MAO Jingwen1), QU Wenjun3), WU Liuling 2,4), Phillip J.UTTLEY2), Tony NORMAN2),ZHENG Jianmin5), QIN Yunzhong4)1)Institute of Mineral Resources,Chinese Academy of Geological Science,Beijing,100037;2)Sino Gold Mining Limited,Sydney,NSW 2000,Australia;3)National Research Center of Geoanalysis,Chinese Academy of Geological Science,Beijing,100037;4)No.271 Geology Team of Guangxi,Lingui,Guangxi,541100;5)China University of Geosciences,Beijing,100083;Re-Os Dating of Arsenian Pyrites from the Lannigou Gold Deposit,Zhenfeng,Guizhou Province,and Its Geological Significances[J];Geological Review;2007-03
8 HE Jinzhong1,2),YAO Shuzhen1),GONG Quansheng3),CHEN Yaoyu3)1) China University of Geosciences,Wuhan,430074; 2) Gansu Institute of Geological Surveying,Lanzhou,730000;3) No.3 Geology and Exploration Team,Gansu Provincial Bureau of Geology and Mineral Exploration and Development,Lanzhou,730000;Genesis of the Dashui Gold Deposit in Maqu,Gansu Province:Evidence from Geochemical Analysis[J];Acta Geologica Sinica;2008-08
9 ZHAO Yuanyi1),SONG Liang2),FAN Xingtao3),SHI Denghua4),ZHANG Tianping4),CHEN Hongqi4),QU Wenjun3)1) Institute of Mineral Resources,CAGS,Beijing,100037;2) China University of Geosciences,Beijing,100083;3) National Analytic Center of Geology,Beijing,100037;4) No.5 Geological Party,Tibet Bureau of Geology and Mineral Exploration and Development,Golmud,Qinghai,816000;Re-Os Dating of Molybdenite from the Shesuo Copper Polymetallic Ore in Shenzha County,Tibet and Its Geological Significance[J];Acta Geologica Sinica;2009-08
10 GE Liang-sheng1,2,4,DENG Jun2,ZHANG Wen-zhao1,LI Qiang-zhi3,ZHANG Yan-chun2,GUO Xiao-dong1,4,LU Yan-ming1(1.Institute of Gold Geology of the Gold Forced Police Army,Langfang 065000,Hebei,China;2.The State Key Lab of Geology and Mineral Resources of China University of Geology,Beijing 100083,China;3.The Gold Headquarter of the Forced Police Army,Beijing 100055,China; 4.The Institute of Geology of the Chinese Academy of Geosciences,Beijing 100037,China);GOLD DEPOSITS IN CHINA(Ⅰ):THE RESENT PROGRESS OF METALLOGENIC THEORY[J];Contributions to Geology and Mineral Resources Research;2008-04
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1 LI Ming Yan, LIU YuLin and LI XiangBo (Institute of Geology and Geophysics, CAS, Beijing 100029, China;Peking University, Beijing 10871, China;Huangshi Institute of Technology, Huangshi 435003, Hubei, China);The determination of the Baolun orogenic gold deposits in Hainan Province[A];[C];2006
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1 HUANG Peng1,2,3, GU Xue xiong4, TANG Ju xing4 and WANG Li quan3(1. Institute of Oceanography, Chinese Academy of Sciences, Qingdao 266071, China; 2. Postgraduate school of the Chinese Academy of Sciences, Beijing 100039, China; 3. Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China; 4. Chengdu University of Technology, Chengdu 610059, China);SOURCES OF ORE FORMING MATERIALS OF THE YULONG PORPHYRY COPPER (MOLYBDENUM) DEPOSIT, TIBET[J];Geotectonica Et Metallogenia;2002-04
2 Shi Yafeng 1 Li Jijun 2 Li Bingyuan 3 Yao Tandong 1 Wang Suming 4 Li Shijie 4 Cui Zhijiu 5 Wang Fubao 6 Pan Baotian 2 Fang Xiaomin 2 Zhang Qingsong 3 1 (Lanzhou Institute of Glaciology and Geocryology, CAS, Lanzhou 730000) 2 (De;UPLIFT OF THE QINGHAI—XIZANG (TIBETAN) PLATEAU AND EAST ASIA ENVIRONMENTAL CHANGE DURING LATE CENOZOIC[J];ACTA GEOGRAPHICA SINICA;1999-01
3 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
4 Liu Ying; Liu Haichen; Li Xianhua (Guangzhou institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640);SIMULTANEOUS AND PRECISE DETERMINATION OF 40 TRACE ELEMENTS IN ROCK SAMPLES USING ICP-MS[J];GEOCHIMICA;1996-06
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6 Feng Xiaoliang 1,2 ,Guan Shiping 1 , Mou Chuanlong 1 , Hou Zengqian 3 ,Li Shengrong 4 (1. Chengdu Institute of Geology and Mineral Resources, Chengdu, 6110082; 2. Chengdu University of Technology, Chengdu,610059; 3.Institute of Mineral Deposits a;GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE JIAMA COPPER-POLYMETALLIC DEPOSIT IN TIBET[J];Geology-geochemistry;2001-04
7 ZHENG You ye,WANG Bao sheng,FAN Zi hui,ZHANG Hua ping( 1.Faculty of Earth Resources,China University of Geosciences,Wuhan Hubei 430074,China; 2.Tibet Bureau of Geology and Mineral Exploration and Development,Lhasa Tibet 858000,China );ANALYSIS OF TECTONIC EVOLUTION IN THE EASTERN SECTION OF THE GANGDISE MOUNTAINS,TIBET AND THE METALLOGENIC POTENTIALITIES OF COPPER GOLD POLY METAL[J];Geological Science and Technology Information;2002-02
8 WANG Xiao-chun,YAN Zi-gui,ZHOU Wei-De,JIA Xiang-kan,LI Zuo-hua,WEN Jun,XU De-zhang,YUAN Jian-fei (Sichuan Institute of Metallurgical Geology & Exploration,Chengdu 610051);PRELIMINARY STUDY ON GEOLOGICAL FEATURES OF PORPHYRY-TYPE COPPER DEPOSITS IN THE NORTHWESTEN NIMU, MIDDLE SECTION OF GANGDISI BELT, TIBET[J];Geology and Prospecting;2002-01
9 Zhang Yuquan Xie Yingwen Qiu Huaning Li Xianhua(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640) Chung Sunlin (Department of Geology, Taiwan University, Taibei 10770);SHOSHONITIC SERIES:Sr,Nd,AND Pb ISOTOPIC COMPOSITIONS OF ORE BEARING PORPHYRY FOR YULONGCOPPER ORE BELT IN THE EASTERN XIZANG(TIBET)[J];;1998-03
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