断裂构造研究的进展和趋势

doi:10.11867/j.issn.1001-8166.1992.06.0025

地球科学进展 ›› 1992, Vol. 7 ›› Issue (6): 25 -. doi: 10.11867/j.issn.1001-8166.1992.06.0025

断裂构造研究的进展和趋势

樊光明朱志澄

中国地质大学武汉 430074

收稿日期:1992-01-24 出版日期:1992-11-01

THE PROGRESS Ale1D TEI}IDENCY OF FAULT RESEARCH

Fan Guangming Zhu Zhicheng

Deyartment of Geology,Clzina University of Geoscienees,Wnhan，430074

Received:1992-01-24 Online:1992-11-01 Published:1992-11-01

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断裂构造是地壳一岩石圈中最重要的构造，是区域构造的格架，既控制了区域构造的发展和横向不均一性，又控制了地壳一岩石圈的分层结构。地壳中的三种构造应力场(挤压、引张和剪切)形成三类断层:挤压性断层、伸展性斯层和走滑性断层，三者既独立存在又相互组合。从三类断层的研究史的回顾和现状分析，概括了其研究进展、趋势及应把握的研究方向。

关键词: 断裂结构, 构造应力场, 挤压性断层, 伸展性断层, 走滑性断层

Fault is the most important type of tectonics in the earth crust一lithosphere. It is the faults，is a dominant elements,SVhich construct regional tectonic architecture. Fault controlled not only the evolution and the transverse inhomogenity of regional tectonics,but also the laminary structure of the earth crust-lithosphere. Three kinds of faults(compressional fault，extensional fault and strike-slip fault) may be formed by three kinds of tectionic stress-fields in the earth crust. The fault might occur individually and combine to each other as well. The recent progress and the tendency of fault research are summarized in this paper from historical review and recent analysis of study in three type fault,in orderto undertand the orentation which must be held.

Key words: Fault structure, Compressional faut, Extensional fault, Strike-slip fault.

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