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台湾岛位于亚州东海陆架边缘。是现代西太平洋沟-弧-盆系的组成部分,居于琉球弧与菲律宾弧的联接处,也是屹立在我国大陆的海岸山脉。从构造部位来看,它北接日本-琉球,南联菲律宾沟-弧-盆系。因此它是西太平洋活动大陆边缘的重要地区。
Taiwan Island is located on the edge of the East China Sea shelves. It is an integral part of the modern Western Pacific ditch-arc-basin system and lives at the junction of the Ryukyu Arc and the Philippine Arc. It is also a coastal mountain range that stands on the mainland of China. From the structural point of view, it north of Japan - Ryukyu, the southern union of the Philippine ditch - arc - basin system. It is therefore an important area on the western edge of the continent of activity.