西南石油大学学报(自然科学版) ›› 1995, Vol. 17 ›› Issue (2): 8-14.DOI: 10.3863/j.issn.1000-2634.1995.02.02

• 地质勘探 • 上一篇    下一篇

黄骅拗陷构造运动程式探讨

刘学锋1 卢顺容2
  

  1. (1.江汉石油学院地质系2.中国地质大学(北京) )
  • 收稿日期:1994-09-29 修回日期:1900-01-01 出版日期:1995-04-20 发布日期:1995-04-20

Discussion on Tectonic Movement Process of Huanghua Depression

Liu Xue-feng1 Lu Shun-rong2   

  1. (1.Dept. of Petroleum Geology,JPI;2.University of Geoscience. Beijing,China)
  • Received:1994-09-29 Revised:1900-01-01 Online:1995-04-20 Published:1995-04-20

摘要:

黄骅拗陷是勃中三叉裂谷系中的一支裂谷,其有地幔隆起,高热流和火山活动频繁有等特征。拗陷中发育着四套构造地层组合,对应着三个构造层次。裂谷盆地的演化经历了三个阶段不同方向的构造运动程式:(1)前裂谷阶段经受印支运动近南北向的挤压作用、燕山早期运动北西—南东向的挤压作用及燕山晚期运动北西西—南东东向的挤压作用等;(2)裂谷阶段经受两期裂陷作用,为北西—南东向和近南北向的引张作用;(3)压裂谷阶段裂谷萎缩引起的垂向下陷运动。

关键词: 裂谷带, 拗陷, 隆起, 构造体系

Abstract:

Huanghua Depression is rift of Bozhong Triple Rifts that have the features of mantle uplift,high—heat flow and strong volcanic activity. Four tectono—stratigraphic units in this depression exist in each of the three tectonic levels. The evolution of the rift basin underwent three periods of tectonic movement patterns with different orientations:①During the pre— rift period,the compressive orientations with S—N direction. NW—SE direction and NWW —SEE direction were produced by the Indo— China Movement,the Early Yanshan Movement and the Late Yanshan Movement respectively;②During the rift period,two phases of rifting with the extensions of NW—SE and S—N direstion were produced in the depression;③During the post—rift period,the tectonic movement changed from horizontal movement to vertical subsidence because of the shrinkage of the rift.

Key words: Rift zone, Depression, Uplift, Tectonic system

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