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《Geotectonica Et Metallogenia》 2006-03
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GEOTECTONIC EVOLUTION BACKGROUND AND ORE-FORMING PROCESS OF Pb-Zn DEPOSITS IN CHUAN-DIAN-QIAN AREA OF SOUTHWEST CHINA

ZHANG Zhibin 1,2, LI Chaoyang1, TU Guangchi1, XIA Bin1 and WEI Zhenquan 1,2 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Graduate School of Chinese Academy of Sciences, Beijing 100039, China)  
The Pb-Zn deposits in the Chuan-Dian-Qian border area in Southwest China, are constrained by geotectonic evolution background, which indicates that the mineralization of the Pb-Zn deposits are related to the two episodes of regional compression that occurred in late Indosinian and Yanshanian epochs, based on analytical results concerning the stress and strain fields associated with Pb-Zn mineralization in Tianbaoshan ore field. The compression in nearly NWW-SEE direction is the main force that led to formation of the regional, NWW-trending extensional faults, and hosting of ore bodies in the end of late Triassic. The regional compression of nearly SSW-NNE direction is also the main cause for the formation of regional, NEE-trending extensional faults, and hosting of ore bodies in Jurassic. So, the late Indosinian and Yanshanian tectonic movements are the main tectonogenetic forces in the study area. Based on regional magmatism and isotopic data concerning diagenesis and mineralization, it is realized that two small-scale magmatism events, occurring in the same time with tectonic stress and strain fields, are concurrent with the Pb-Zn mineralization, so it is possible that these two magmatism events may have provided partial metallogenic materials and geothermal energy for the mineralization. The Pb-Zn mineralization in this area is the results of collision between Yangtze plate and LanpingSimao block and between Yidun island arc belt and Yangtze plate at the end of late Triassic, and the opening and expansion of Yaluzangbu Paleo-ocean in early Jurassic. These two main tectonic-active episodes, and the regional tectono-magmatism geothermal events are synchronic with the mineralization. Based on some isotopic ore-forming age results published recently, it is found that the age data for these actions are concentrated in 226~225Ma and 176.5±2.5Ma. So, this area underwent two main Pb-Zn mineralizing periods, i.e., late Triassic and early Jurassic.
【Fund】: 国家重点基础研究发展规划项目(2001CB409805)资助;; 中科院创新重要方向性项目(KZCX3SW137)联合资助.
【CateGory Index】: P618.42;P618.43
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7 SONG Chunyan1,2, WANG Jian2, FU Xiugen2, CHEN Ming2 and HE Li2 (1.Graduate Department of the Chinese Academy of Geological Sciences, Beijing 100037, China;2.Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China);Structural Characteristics and its Petroleum Geological Significance of the Boerzanglongba Anticline in the Qiangtang Basin,Northern Tibetan Plateau,China[J];Geotectonica Et Metallogenia;2012-01
8 Wan Li,Zhao Zeheng (Research Institute of South Company,SINOPEC,Chengdu,Sichuan 610041);Reservoir characteristics of Devonian Permian organic reef shoal in Nanpanjiang and its control factors[J];Complex Hydrocarbon Reservoirs;2013-01
9 WANG Jue1,LIU Jin-hai2,CHEN Yun-ming2(1.The Bureau of Land and Resource Zunyi,Zunyi 563000,Guizhou,China;2.Geologic Party 102, Guizhou Bureau of Geology & Mineral Exploration and Development,Zunyi 563003,Guizhou,China);REE Geochemical Characters of Hydrothermal Dolomite of Dengying Formation of Sangmuchang Anticline in North Guizhou[J];Guizhou Geology;2013-02
10 LV Xian-he1,GAO Ting-chen1,CHEN Jun-kui1,CHEN Rui-bao1,CHENG Xing-guo2,HU Xiao-chuan2,CAI Zhong-ming2(1.Henan Institute of Geological Survey,Zhengzhou 450051,China;2.Henan Team of Regional Geological Survey,Zhengzhou 450051,China);Geological characters of gypsum deposit and its indicating significance to sulfide deposits[J];Journal of Geology;2011-01
【Secondary Citations】
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1 Wang Zhenmin;RELIABILITY OF SOME GEOCHRONOLOGICAL DATA FOR KANG-DIAN AXIS, SICHUAN[J];;1987-01
2 Wu Genyao (Institute of Geology, Academia Sinica);TECTONIC EVOLUTION OF PANZHIHUA XICHANG PALEORIFT DURING LATE PALAEOZOIC[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;1997-02
3 HUANG Zhilong1, LI Wenbo1, CHEN Jin2, XU Deru1,4, HAN Runsheng3 and LIU Chongqiang1 (1. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, C hina; 2. Huize Pb-Zn Mine of Yunnan, Huize 654211, China; 3. Kunming University of Science and Technology, Kunming 650093, China; 4. Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry &South China Sea Institute of Oceanology, Chinese Academy of Science, Guangzhou 510640, China);CARBON AND OXYGEN ISOTOPE GEOCHEMISTRY OF THE HUIZE SUPERLARGE Pb-Zn ORE DEPOSITS IN YUNNAN PROVINCE[J];Geotectonica Et Metallogenia;2004-01
4 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
5 ZHANG Yue-qiao 1 ,YANG Nong 1 ,MENG Hui 2 ,CHEN Wen 3 (1.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing100081,China;2.China Institute of Geological Environment Measurement,Beijing100081,China;3.Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Late Cenozoic tectonic deformation history and uplift process of the Panxi region,western Sichuan[J];Chinese Geology;2004-01
6 HE Bin 1,2 ,WANG Ya-mei 2 ,JIANG Xiao-wei 1(1.Guangzhou Institute of Geochemistry,Chinese Academy of Science,Guangzhou510640,China;2.China University of Geosciences,Wuhan430030,Hubei,China);Paleo-karst landforms on top of limestone of the Maokou Formation in the west of the Upper Yangtze platform and its geological significance[J];Chinese Geology;2004-01
7 XU Yi-Gang1, CHUNG Sun-Lin2 (1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. Department of Geology, National Taiwan University, Taibei, China);The Emeishan Large Igneous Province: Evidence for mantle plume activity and melting conditions[J];Geochimica;2001-01
8 LI Xian-hua 1 ,ZHOU Han-wen 1 ,LI Zheng-xiang 2 ,LIU Ying 1 ,P.Kinny 3 (1.Guangzhou Institute of Geochemistr y,Chinese Academy of Sciences,Guangzhou510640,China;2.Tectonic Special Research Centre,Department of Geology and Geo;Zircon U-Pb age and petrochemical characteristics of the Neoproterozoic bimodal volcanics from western Yangtze block[J];Geochimica;2001-04
9 LIANG Xi rong, WEI Gang jian, LI Xian hua, LIU Ying(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China);Precise measurement of ~(143)Nd/~(144)Nd and Sm/Nd ratios using multiple collectors inductively coupled plasma mass spectrometer (MC ICPMS)[J];Geochimica;2003-01
10 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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