俯冲作用控制的日本海构造活动与演化的数值模拟
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摘要
<正>由新生代海沟-岛弧-盆地复合体系所构成的岛弧型活动大陆边缘主要分布在亚洲大陆东部的太平洋西岸,北起俄罗斯的萨哈林岛、经日本列岛向南延伸至琉球群岛、我国的台湾岛及其南缘的菲律宾群岛,该区域内沉积作用、岩浆活动、构造作用和成矿作用活跃,且与板块的生长和消亡密切相关(郭令智等,1985)。其中尤以日本海最为典型。日本岛周围有四个板块:阿穆利亚板块、菲律宾板块、鄂
引文
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