天然气地质学

对渤海湾盆地张扭、压扭性构造的一点认识

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  • [1]中科院广州地化所边缘海地质重点实验室; [2]华南理工大学化学工程学院; 广东广州; [3]中国科学院研究生院

收稿日期: 2006-02-21

  修回日期: 2006-04-22

  网络出版日期: 2006-08-20

AN UNDERSTANDING OF TENSE-SHEARING AND COMPRESSO-SHEARING STRUCTURES IN BOHAI BAY BASIN

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  • 1.Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;2.Graduate School of the Chinese Academy of Sciences,Beijing 102249,China;3.Institute of Chemical South China University of Technology,Guangzhou 510640,China

Received date: 2006-02-21

  Revised date: 2006-04-22

  Online published: 2006-08-20

摘要

张扭和压扭性构造是兼有走滑和拉张挤压2种作用的构造样式。经对大量具有张扭和压扭特征断层的统计提出,这2种扭动断层在沉积盆地的发育中具有特殊的空间位置与剖面特征,认为应当进一步加深对张扭和压扭断层的研究和认识,张扭和压扭构造是厘定渤海湾盆地及其内部坳陷演化过程的必需条件。

本文引用格式

于俊峰;夏斌;许静; . 对渤海湾盆地张扭、压扭性构造的一点认识[J]. 天然气地球科学, 2006 , 17(4) : 473 -476 . DOI: 10.11764/j.issn.1672-1926.2006.04.473

Abstract

The structural manner studying provides a crucial presumption of tectonic movement and developing processes.Tense-shearing and compresso-shearing structure accompanies two types of structural manners with striking and extending and contrcting action.A static coming from abundance of tense-shearing and compresso-shearing faults indicates that the two types of faults have specific spacial and profiling characters in sedimentary basins.What means that the former discerning of tense-shearing and compresso-shear.

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