Geological role of Tuluanshan-Huatung fault in developing the Coastal Range,Taiwan arc-continent col

• 作 者: Chi-YueHuang[1]Chung-PaiChang[2]Ching-WeeiLin[1]Chih-WeiChien[1]
• 机 构: Department of Earth Sciences, National Cheng Kung University, Tainan
• 出 处: 海峡两岸第七届海洋科学研讨会
• 发表日期: 2008年期

@@Due to a southward propagation of the collision between the underthrusting Eurasian continent and the NW-moving Luzon arc, marine geology off SE Taiwan not only displays the active collision tectonics but also provides a modern analog of the Coastal Range before its final arc-forearc accretion in the last 2 Ma (Fig. 1; Huang et a; 1992, 2000, 2006). Accordingly, W-E seismic profiles in the active collision zone off SE Taiwan and structural cross-sections over the Coastal Range from the south to the north would show the structural evolution of the Coastal Range.