ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西南三江地区造山演化过程及成矿时空分布
  
关键词:Archipelago orogenesis  intracontinental subduction orogenesis  intracontinental transform orogenesis  metallogenic time-space distribution
基金项目:大规模成矿作用及大型矿集区预测”项目(G1999043203)
作者单位
骆耀南 四川省地质矿产勘查开发局成都610081 
俞如龙 四川省地质矿产勘查开发局成都610081 
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摘要:
Orogenic Evolution and Metallogenic Time-Space Distribution in Jinshajiang-Lancangjiang-Nujiang Region,Southwest China
      Geology of Jinshajiang Lancangjiang Nujiang region in Southwest China cannot be satisfactorily interpreted by the hypothesis"one orogenesis". An interpretation of "polyphase orogenesis" and "polyphase metallogenesis" has been proposed in the paper. Du ring the Late Palaeozoic Early Mesozoic archipelago orogenic stage, Qiangtang, Jomda and Lincang arcs should have served as the frontal arc, behind which a series of back arc basins and island arcs or remnant arcs (or microcontinents) was distributed. In the Middle Late Mesozoic orogenic stage of intracontinental subduction, Jinshajiang, Ailaoshan and Longmenshan Jinpingshan belts might have acted as the main intracontinental subduction zone, which caused the formation of Yanshanian remelting granites and controlled the distribution of mineral resources. In the Cenozoic stage of intracontinental transform orogenesis, the characteristic tectonic magmatic metallogenic zone was developed, which has a potential for the formation of large or superlarge deposits.
LUO Yao-nan,YU Ru-long.2002.Orogenic Evolution and Metallogenic Time-Space Distribution in Jinshajiang-Lancangjiang-Nujiang Region,Southwest China[J].Acta Geoscientica Sinica,23(5):417-422.
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