| 昌马断裂带断层岩研究及其粘滑,蠕滑特征 |
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| 引用本文： | 吕德徽 侯康明. 昌马断裂带断层岩研究及其粘滑,蠕滑特征[J]. 内陆地震, 1995, 9(1): 29-34 |
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| 作者姓名： | 吕德徽 侯康明 |
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| 作者单位： | 国家地震局兰州地震研究所 |
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| 摘 要： | 在对断层岩的分布、内部结构、宏观变形及断层泥中石英颗粒形态、表面特征研究分析的基础上，讨论了昌马断裂带粘滑、蠕滑特征。同时指出，昌马断裂带虽以粘滑运动为主，但仍伴有一定量的蠕滑活动。
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| 关 键 词： | 北祁连山 断裂带 断层岩 断层滑动 地震预报 |
STICK AND CREEPING SLIP AND FAULT ROCKS OF CHANGMA FRACTURE ZONE |
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| Lu Dehui,Hou Kangming. STICK AND CREEPING SLIP AND FAULT ROCKS OF CHANGMA FRACTURE ZONE[J]. Inland Earthquake, 1995, 9(1): 29-34 |
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| Authors: | Lu Dehui Hou Kangming |
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| Abstract: | On the analysis of the spreadings, internal structure,macrodeformation of the fault rocks and quartz grain shapes in and on the fault gauge,behaviors of stick and creeping slips happened on Changma fracture zone were discussed,indicating that although being principally characterized by stick slip movement, Changma fracture zone is still having certain movement of creepings. |
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| Keywords: | Fracture zone on the northern Qilianshan Fault rock Fault slip Earthquake prediction Seismic intensity regionalization |
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