海陆断裂带(COFZs)是大陆裂谷时期和海洋扩张初期发育的构造板块边界的一个基本类型。通过动力模式研究,我们发现它们有3个主要的形成过程:陆—陆剪切、洋壳增生以及伴随的COFZ沿线的海陆剪切过程(Le Pichon和Hayer,1971;Scrutton,1979;Mascle和Blarez,1987);然而,有关古COFZs Sea-continent fault zones (COFZs) are a basic type of tectonic plate boundaries developed during the continental rifting and early marine expansion. We found that they have three major formation processes through dynamic mode studies: land-land shear, oceanic shell growth and accompanying sea-land shear processes along the COFZ (Le Pichon and Hayer, 1971; Scrutton, 1979; Mascle and Blarez , 1987); however, related to the ancient COFZs