发展板块构造:从洋壳俯冲到大陆碰撞

被引：20

作者：

郑永飞 ^{[1
]}

叶凯 ^{[2
]}

张立飞 ^{[3
]}

机构：

[1] 中国科学院壳幔物质与环境重点实验室,中国科学技术大学地球和空间科学学院

[2] 岩石圈演化国家重点实验室,中国科学院地质与地球物理研究所

[3] 造山带与地壳演化教育部重点实验室,北京大学地球与空间科学学院

来源：

科学通报 | 2009年 / 54卷 / 13期

关键词：

地壳俯冲; 大陆碰撞; 超高压变质; 大陆动力学;

D O I：

暂无

中图分类号：

P542 [构造运动];

学科分类号：

摘要：

大陆地壳深俯冲与超高压变质的研究不仅带动了中国固体地球科学的发展,而且为发展板块构造理论提供了契机.根据俯冲地壳的性质,已经认识到俯冲和碰撞分别以两种类型出现.就地壳俯冲来说,存在洋壳俯冲型(例如太平洋周边)和陆壳俯冲型(例如阿尔卑斯造山带).就大陆碰撞来说,则存在弧-陆碰撞型(例如喜马拉雅和青藏造山带)和陆-陆碰撞型(例如大别-苏鲁造山带).大陆俯冲带深部化学变化与差异折返、洋壳俯冲与陆壳俯冲之间的时空转换,将是今后一个时期大陆动力学研究的重点.

引用

页码：1799 / 1803

页数：5

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