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1前言台湾山脉是世界最年青山脉之一。关于该碰撞带已提出三种主要假说：1）Suppe（1981）的薄皮构造模式，在该模式中，吕宋弧与欧亚陆缘碰撞。2）Lu和HSS（1992）的模式，该模式是指一外来块体首先与欧亚陆缘碰撞，接着吕宋弧与已经增生的外来决体第二次碰撞。3）Hsu和Sibuet
1 Introduction Taiwan’s mountains are one of the youngest mountains in the world. Three major hypotheses have been proposed regarding this collision zone: 1) Thin-skinned structural model of Suppe (1981), in which the Luzon arc collides with the Eurasian continental margin. 2) The model of Lu and HSS (1992), which means that a foreign body first collided with the Eurasian continental margin, followed by a second collision between the Luzon arc and an already proliferating clan. 3) Hsu and Sibuet