华北岩石圈减薄与克拉通破坏研究的主要学术争论

被引:477
作者
吴福元 [1 ]
徐义刚 [2 ]
高山 [3 ]
郑建平 [3 ]
机构
[1] 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室
[2] 中国科学院广州地球化学研究所中国科学院同位素年代学和地球化学重点实验室
[3] 中国地质大学(武汉)地质过程与矿产资源国家重点实验室
关键词
岩石圈减薄; 克拉通破坏; 华北;
D O I
暂无
中图分类号
P542 [构造运动];
学科分类号
070904 ;
摘要
华北岩石圈减薄是近十年来国内外研究的热门课题,但关于岩石圈减薄的具体时间、减薄幅度、空间分布范围、机制及其构造控制因素,多有争论。本文对上述问题进行了全面的回顾与讨论,内容包括:(1)是克拉通破坏还是岩石圈减薄;(2)古生代以来华北克拉通岩石圈地幔时代与壳幔解耦;(3)岩石圈减薄与克拉通破坏发生的时间;(4)岩石圈减薄的垂向幅度;(5)克拉通破坏在中国东部的空间分布;(6)克拉通破坏机制;(7)克拉通破坏的地球动力学原因;(8)华北克拉通破坏在世界上的特殊性等。文后,汇编了近10余年来华北岩石圈减薄与克拉通破坏研究的重要文献。
引用
收藏
页码:1145 / 1174
页数:30
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