青藏高原多岛弧-盆系格局机制  

THE FRAME MECHANISM OF MULTIPLE ISLAND ARC-BASIN SYSTEM IN TIBETAN PLATEAU

作　　者：潘桂棠[1] 徐强[1] 王立全[1] 

机构地区：[1]中国地质调查局青藏高原地质研究中心,四川成都610082

出　　处：《矿物岩石》2001年第3期186-189,共4页Mineralogy and Petrology

摘　　要：本文根据长期的青藏高原及周边地区的地质调查和考察实践 ,在系统研究全球构造 ,尤其是特提斯地质的基础上 ,概要阐述了全球洋 -陆构造体制的转换论、多岛弧盆系统论、造山作用过程论 ,并依此“三论”After long term geological survey and practice in the Tibetan Plateau and its surrounding areas and based on the systematic study on the global structure,especially on Tethyan geology,we briefly dissussed the transform theory of global ocean continent frame system,the system theory of multiple island arc basin and the process theory of orogenesis,which were regarded as the basis of classsifying the geotectonic units of the Tibetan Plateau and its surrounding areas.

关 键 词：青藏高原 转换论 系统论 过程论 多岛弧-盆系 造山作用 

分 类 号：P548.2[天文地球—构造地质学]