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贺兰山西麓断裂右旋走滑的地质地貌证据及其构造意义
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雷启云1, 张培震2,3, 郑文俊3, 杜鹏1, 王伟涛2, 俞晶星2, 谢晓峰1 |
GEOLOGICAL AND GEOMORPHIC EVIDENCE FOR DEXTRAL TRIKE SLIP OF THE HELAN SHAN WEST-PIEDMONT FAULT ND ITS TECTONIC IMPLICATIONS
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LEI Qi-yun 1, ZHANG Pei-zhen 2,3, ZHENG Wen-jun 3, DU Peng 1, WANG Wei-tao 2, YU Jing-xing 2, XIE Xiao-feng 1
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走滑断层及其派生节理和小褶皱示意图( 据朱志澄, 1999 ) F 主断层; σ 1派生应力场主压应力轴; σ 2派生应力场主张应力轴; S1, S2剪节理;T 张节理; D 小褶皱面; 右下图为应变椭球体 |
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