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

下载PDF ( 731 )

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.

[1]朱志澄.构造地质学的新进展及新构造观.地质科技情报，7988,7(1)

[2]马杏垣.构造解析学当议.地球科学，1983>(3)

[3]Bruhn,R L. Continental Tectonics ;Selected Topices. Rewiews of Geophysics, 1987,25(6)

[4]Boyer,S E et a1. Thrust Systems. AAPG Bull. 1982,66(9)

[5]Sibson,R H. Fault Rocks and Fault Mechanisms. Journal o# Gelological Society,London, 133

[6]Toshihiko Shimamoto(岛本年彦)(樊光明译). S-C糜棱岩的成因和一种新的断层带模式地质科学译丛,1990(1)

[7]Dahlatrom,C D A. Balanced cross Sections. Canadian Journal of Earth Seience,1969(6);F743-757

[8]Chapman,T Jet a1. Displacement一distance Method in the Analysis of Fold一thrust structure and Linked一fault Systems. Journal of Geological society，1984(141)

[9]Malavieille,J et al. Kinematic Model for Postorogenic Basin and Range Extension. Geology, 1991,19,P555一558

[10]Spcncer,J E et al. Possible Controls of Base一and precious一Metal Mineralization Associted with Tertiary Detacnment Fault in the Lower Colorado River trough Arizona and California. Ceology,1986,19

[11]Lister,C et al(李志锋译)币和展构造新模式及对澳大利亚找金的意义.国外地质矿产，1987(1)

[1]	解国爱，王宗秀，张庆龙，吕赟珊，邹旭. 江西永平铜矿区古构造应力场与构造演化[J]. 地球科学进展, 2013, 28(5): 608-617.
[2]	钟广法，游倩. 高分辨率FMS成像测井资料在科学大洋钻探中的应用[J]. 地球科学进展, 2012, 27(3): 347-358.
[3]	罗胜元，何生，王浩. 断层内部结构及其对封闭性的影响[J]. 地球科学进展, 2012, 27(2): 154-164.
[4]	张明利，万天丰. 含油气盆地构造应力场研究新进展[J]. 地球科学进展, 1998, 13(1): 38-43.

阅读次数

全文

摘要