石油与天然气地质 ›› 2013, Vol. 34 ›› Issue (6): 841-846.doi: 10.11743/ogg20130619

• 技术方法 • 上一篇    下一篇

塔里木盆地雅克拉断凸古构造应力场数值模拟

罗小龙1,2,3, 汤良杰1,2   

  1. 1. 中国石油大学 油气资源与探测国家重点实验室, 北京 102249;
    2. 中国石油大学 盆地与油藏研究中心, 北京 102249;
    3. 长江大学 地球科学学院, 湖北 武汉 430100
  • 收稿日期:2013-07-19 修回日期:2013-11-08 出版日期:2013-12-08 发布日期:2014-01-04
  • 作者简介:罗小龙(1974- ),男,博士研究生,含油气盆地构造解析。E-mail:lxl2001181@163.com。
  • 基金资助:
    国家自然科学基金项目(41172125);中石化西北油田分公司项目(KY2010-S-053,KJ2008-29)。

Numerical simulation of palaeotectonic stress field in Yakela faulted salient, the Tarim Basin

Luo Xiaolong1,2,3, Tang Liangjie1,2   

  1. 1. State Key Laboratory for Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China;
    2. Basin & Reservoir Research Center, China University of Petroleum, Beijing 102249, China;
    3. School of Geosciences, Yangtze University, Wuhan, Hubei 430100, China
  • Received:2013-07-19 Revised:2013-11-08 Online:2013-12-08 Published:2014-01-04

摘要: 雅克拉断凸长期处于挤压环境,逆断层发育,但在喜马拉雅早期正断层也发育。为了研究雅克拉断凸的断层发育特征,对海西晚期和喜马拉雅早期古构造应力场进行三维有限元数值模拟。结果表明,海西晚期整个研究区在挤压应力作用下皆为中、低应力值区,中、东部南侧是低应力值区,往北、往西应力值增加,该应力场导致研究区内部发育了一些规模较小的逆断层。喜马拉雅早期研究区在挤压应力作用下向上隆起,隆起幅度由西向东逐渐增加,隆起导致地层弯曲,且以边界断裂顶部附近区域弯曲度最大,导致此处的拉张应力也最大,正断层正是从此处开始发育,然后再向内发展;与此同时,研究区下部受到的挤压应力作用较小,导致内部的逆断层几乎没有进一步发育 。

关键词: 海西晚期, 喜马拉雅早期, 数值模拟, 构造应力场, 雅克拉断凸, 塔里木盆地

Abstract: Thrust faults are widely developed in Yakela faulted salient due to long-term compression regime.However,some normal faults were also formed during the Early Himalayanian.In order to decode the mechanism of formation and evolution of these faults,we conducted 3D finite element numerical simulation for the Late Hercynian and Early Himala-yan stress field in the Yakela faulted salient.During the Late Hercynian,the compressive stress resulted in the low stress areas in the central and eastern parts of the Yakela faulted salient and the low to moderate stress in the west and north part.This stress field caused the development of some small-scale thrust faults in the Yakela faulted salient.During the Early Himalayan,the compressive stress induced uplifting of the study area,with the amplitude of uplifting increasing from west to east.As a result,the strata bended in the study area,with the strongest tensile stress occurring on top of the boundary fault,and normal faults were also developed in these locations and extended inwards.Meanwhile,compression stress was weak in the lower part of the whole study area,thus did not induce the further development of thrust faults in the inner parts of the study area.

Key words: Late Hercynian, Early Himalayan, numerical simulation, tectonic stress field, Yakela faulted salient, Tarim Basin

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