从多岛弧盆系研究实践看板块构造登陆的魅力  

Charm of landing of plate tectonics on the continent as viewed from the study of the archipelagic arc-basin system

作　　者：潘桂棠[1,2] 王立全[1,2] 尹福光[1,2] 朱弟成[1,2] 耿全如[1,2] 廖忠礼[1,2] 

机构地区：[1]中国地质调查局成都地质矿产研究所,四川成都610082 [2]中国地质调查局青藏高原地质研究中心,四川成都610082

出　　处：《地质通报》2004年第9期933-939,共7页Geological Bulletin of China

基　　金：国家973项目<印度与亚洲大陆主碰撞成矿带作用>(编号:2002CB412600)下属课题<成矿潜力评估与战略新区预测>(编号:2002CB412609);<青藏高原南部空白区基础地质综合研究>(编号:200313000025);中国地质调查局<青藏高原及邻区1:150万地质图编制>项目(编号:20031300

摘　　要：板块构造学说是高度成功的地球科学理论。大洋岩石圈与大陆岩石圈之间的多岛弧盆系构造域是板块构造登陆的入门向导。青藏高原大地构造研究实践表明,青藏高原是板块构造登陆的研究基地。众多蛇绿岩带、混杂岩带和火山岩浆弧带等的识别,支持洋陆转换多岛弧盆系构造模式,可用来解释特提斯和亚洲大陆的形成和演化。The theory of plate tectonics is one of the highly successful theories in the geosciences. The rudimental guide of the plate-tectonic theory landing on continent is the archipelagic arc-basin system between the oceanic lithosphere and continental lithosphere. The study of tectonics on the Qinghai-Tibetan Plateau indicates that the Qinghai-Tibetan Plateau is the ideal research base of the plate-tectonic theory landing on the continent. The evolution of the Tethys and formation and evolution of the Asian continent can be interpreted by the tectonic model of the archipelagic arc-basin system in the process of transition between oceanic crust and continental crust, which is supported by the recognition of numerous ophiolitic belts, mélange zones and volcanic-magmatic arcs on the Qinghai-Tibetan Plateau and adjacent regions.

关 键 词：板块构造 洋陆转换 多岛弧盆系 登陆 青藏高原 

分 类 号：P542.4[天文地球—构造地质学]