云南香格里拉地区深部成矿远景分析
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摘要
<正>三江地区是我国重要的有色金属和贵金属成矿远景区,香格里拉位于三江构造带中段,处于峨眉山大火成岩省的外带,但靠近地幔柱中心宾川—丽江—仁川三角地带~([1~3]),分布有大量的与地幔柱作用有关的二叠系玄武岩,经历过强烈的火山作用和构造活动,为有色金属和贵金属造就了十分有利的成矿条件,现已查探明有多个Au,Pb,Zn,Mo等的矿床或矿点。1深部成矿作用概述起源于地核及地幔或俯冲板块的脱水脱气作用
引文
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[2]Li Hongbo,Zhang Zhaochong,Lv Linsu.Geometry of the mafic dyke swarms in Emeishan Large Igneous Province:Implications for Mantle Plume[J].Acta Petrologica Sinica,2010,26(10):3 142-3 152.[李宏博,张招崇,吕林素.峨眉山大火成岩省基性墙群几何学研究及对地幔柱中心的指示意义[J].岩石学报,2010,26(10):3 142-3 152.]
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[6]Mao Jingwen,Li Xiaofeng.Mantle-derived Fluids in Relation to Ore-forming and Oil-forming Processes[J].Mineral Deposits,2004,23(4):520-532.[毛景文,李晓峰.深部流体及其与成矿成藏关系研究现状[J].矿床地质,2004,23(4):520-532.]
[7]Liu Xianfan,Liu Jiaduo,Zhang Chengjiang,et al.The processes of Mantle Plume and mantle fluid and their applying study for the deep prospecting[J].Advance in Earth Sciences,2004,19(S1):93-101.[刘显凡,刘家铎,张成江,等.地幔柱和地幔流体作用与深部找矿应用研究[J].地球科学进展,2004,19(S1):93-101.]
[8]Xiao Long.Plume tectonics and mantle dynamics:On their records in chinese continent[J].Bulletin of Mineralogy Petrology and Geochemistry,2004,23(3):239-245.[肖龙.地幔柱构造与地幔动力学——兼论其在中国大陆地质历史中的表现[J].矿物岩石地球化学通报,2004,23(3):239-245.]
[9]Hu Ruizhong,Tao Yan,Zhong Hong,et al.Mineralization system of Mantle Plume:A case study on Emeishan Mantle Plume[J].Earth Science Frontiers,2005,12(1):42-54.[胡瑞忠,陶琰,钟宏,等.地幔柱成矿系统:以峨眉山地幔柱为例[J].地学前缘,2005,12(1):42-54.]
[2]Li Hongbo,Zhang Zhaochong,Lv Linsu.Geometry of the mafic dyke swarms in Emeishan Large Igneous Province:Implications for Mantle Plume[J].Acta Petrologica Sinica,2010,26(10):3 142-3 152.[李宏博,张招崇,吕林素.峨眉山大火成岩省基性墙群几何学研究及对地幔柱中心的指示意义[J].岩石学报,2010,26(10):3 142-3 152.]
[3]Zhang Zhaochong,Hao Yanli,Wang Fusheng.Picrites in large igneous provinces and their implications[J].Earth Science Frontiers,2003,10(3):105-114.[张招崇,郝艳丽,王福生.大火成岩省中苦橄岩的研究意义[J].地学前缘,2003,10(3):105-114.]
[4]Liu Congqiang,Huang Zhilong,Li Heping,et al.The geofluid in the mantle and its role in ore-forming processes[J].Earth Science Frontiers,2001,8(4):232-243.[刘丛强,黄智龙,李和平,等.地幔流体及其成矿作用[J].地学前缘,2001,8(4):232-243.]
[6]Mao Jingwen,Li Xiaofeng.Mantle-derived Fluids in Relation to Ore-forming and Oil-forming Processes[J].Mineral Deposits,2004,23(4):520-532.[毛景文,李晓峰.深部流体及其与成矿成藏关系研究现状[J].矿床地质,2004,23(4):520-532.]
[7]Liu Xianfan,Liu Jiaduo,Zhang Chengjiang,et al.The processes of Mantle Plume and mantle fluid and their applying study for the deep prospecting[J].Advance in Earth Sciences,2004,19(S1):93-101.[刘显凡,刘家铎,张成江,等.地幔柱和地幔流体作用与深部找矿应用研究[J].地球科学进展,2004,19(S1):93-101.]
[8]Xiao Long.Plume tectonics and mantle dynamics:On their records in chinese continent[J].Bulletin of Mineralogy Petrology and Geochemistry,2004,23(3):239-245.[肖龙.地幔柱构造与地幔动力学——兼论其在中国大陆地质历史中的表现[J].矿物岩石地球化学通报,2004,23(3):239-245.]
[9]Hu Ruizhong,Tao Yan,Zhong Hong,et al.Mineralization system of Mantle Plume:A case study on Emeishan Mantle Plume[J].Earth Science Frontiers,2005,12(1):42-54.[胡瑞忠,陶琰,钟宏,等.地幔柱成矿系统:以峨眉山地幔柱为例[J].地学前缘,2005,12(1):42-54.]
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