ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
滇西兰坪—思茅盆地构造转换机制及成矿响应
  
关键词:tectonic transformation  continent rift  metallogenic  Lanping–Simao basin  eastern Tibetan Plateau  tethys evolution
基金项目:由十一五科技支撑项目(编号: 2006BAB01A07);国家自然科学基金项目(编号: 41202057);中国地质调查局地质大调查项目(编号: 1212011220870; 12120114077201);中央公益性院所基金项目(编号: K1327)
作者单位E-mail
李以科 中国地质科学院矿产资源研究所 like430@qq.com 
王安建 中国地质科学院矿产资源研究所 ajwang@cags.ac.cn 
摘要点击次数: 4937
全文下载次数: 3063
摘要:
The Tectonic Transformation Mechanism and Metallogenic Response of the Lanping–Simao Basin
      The Lanping–Simao basin in the center of San-jiang (Three Rivers) region, located in the southeast-ern margin of the Tibetan Plateau, is tectonically in the transition zone between the Gondwana and Eura-sia tectonic domains. It is also the frontier zone of northeastern extrusion of Indian plate towards the Eurasia plate as well as the escape zone for the deep material. Extensive metallogenesis occurred in the geology epochs due to the sophisticated geological process. Numerous ore deposits of diverse genetic types and metal speciation were formed in Cenozoic, making the Sanjiang one of the most productive and potential regions for metal resources in China. The Cu, Co, Pb, Cr, and Zn resource reserves accounts for 40%、55.7%、29.8%、80%and 30.8% of the total reserves, respectively. The Au, PGE and REE reserves were almost one half of that in china.
LI Yi-ke,WANG An-jian.2017.The Tectonic Transformation Mechanism and Metallogenic Response of the Lanping–Simao Basin[J].Acta Geoscientica Sinica,38(s1):11-14.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: