地质论评2013，Vol.59Issue(1)：129-136,8.
台湾东部海岸山脉对弧陆碰撞的响应
A Review on Response of Arc-continent Collision in Coastal Range,Eastern Taiwan Island
摘要
Abstract
Taiwan Island is situated in the active subduction-collision region between the Eurasian continent and the Philippine Sea plate. Tectonics in the Taiwan region is characterized by two opposite subduction systems; Manila subduction system and Ryukyu subduction system. The uplift of Taiwan results from the oblique collision of the Luzon arc and Eurasian margin. All of the geology characteristics attracted geologists all over the world. The Coastal Range is the onshore portion of the Luzon arc and is composed of deformed and accreted volcanic islands, intra-arc basins and forearc basins. Here we review geochronology, geochemistry, tectonic and geology research results of the Coastal Range and summarize the features of its uplift and erosion. We indicate the main research problems of the Coastal Range in the recent years. Meanwhile, some research directions about geology in the Coastal Range should be emphasized in the future, e. g. how the Lichi melange formed, the affiliation of the crust of the Huatung Basin, the process of the arc-continent collision recorded in tuff in the volcanoes and forearc basins.关键词
台湾/海岸山脉/弧陆碰撞/斜向碰撞/吕宋岛弧Key words
Taiwan/ Coastal Range/ arc-continent collision/ oblique collision/ Luzon arc引用本文复制引用
耿威,张训华,温珍河,黄奇瑜,高志清..台湾东部海岸山脉对弧陆碰撞的响应[J].地质论评,2013,59(1):129-136,8.基金项目
本文为国家地质调查专项"中国海陆地质地球物理及地球化学系列图"项目(编号GZH200900504)成果. （编号GZH200900504）
