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松辽盆地大庆长垣中浅层断层形成演化的新模式
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  • 英文篇名:A new model for the formation and evolution of middle-shallow faults in the Daqing placanticline,Songliao basin
  • 作者:黄磊 ; 童亨茂 ; 杨东辉 ; 范晋煜 ; 黄浩天
  • 英文作者:HUANG Lei;TONG Hengmao;YANG Donghui;FAN Jinyu;HUANG Haotian;State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum;
  • 关键词:大庆长垣 ; 断裂系统 ; 先存断裂 ; 递进变形 ; 应力机制
  • 英文关键词:Daqing placanticline;;fault system;;pre-existing faults;;progressive deformation;;tectonic stress mechanism
  • 中文刊名:DZXE
  • 英文刊名:Acta Geologica Sinica
  • 机构:中国石油大学(北京)油气资源与探测国家重点实验室;
  • 出版日期:2019-03-15
  • 出版单位:地质学报
  • 年:2019
  • 期:v.93
  • 基金:国家自然科学基金项目(编号41272160);; 国家油气重大专项(编号2016ZX05024-005-004)资助成果
  • 语种:中文;
  • 页:DZXE201903006
  • 页数:9
  • CN:03
  • ISSN:11-1951/P
  • 分类号:91-99
摘要
松辽盆地油气集中富集的中浅层断层十分发育,不同反射界面断层发育存在差异,前人认为是多期构造活动的结果。本文应用先存构造条件下断层作用模式,利用三维地震资料,对中浅层的断裂系统重新进行构造解析。结果表明,①松辽盆地大庆长垣中浅层断裂系统按照错断层位、断距、延伸长度、走向可划分为8个类型;②T_2、T_1、T_(06)反射层断层的平均走向分别为322°、320°和316°,断层平均走向从下往上存在逆时针旋转的变化趋势;③大庆长垣自中浅层形成以来,构造应力机制由泉头组—明水组沉积时期的伸展应力机制转变为明水组沉积末期的走滑应力机制,但构造应力场的主应力方向没有发生改变;④研究区复杂的断裂系统是在构造应力场主应力方向保持相对稳定的条件下、在递进变形过程中逐渐形成的。该断层形成演化的新模式更合理地揭示了松辽盆地中浅层断层发育规律和成因机制,对研究区进一步的勘探开发有指导意义。
        The middle-shallow faults, which host a large amount of concentrated oil and gas, are well developed in the Songliao Basin. There exist some differences in development of faults on different reflection interfaces. Previous studies believed they were the products of multi-stage tectonic activities. Based on the modes of faulting in the conditions of previous existing structures, this study analyzed the middle-shallow faulting system using 3 D seismic data. The result shows that:(1) the middle-shallow faulting system of the Daqing placanticline in the Songliao basin can be divided into eight types based on faulted successions, displacements, extents and strikes;(2) the average strikes of faults for T_2, T_1 and T_(06) reflection interfaces are 322°, 320° and 316°, respectively, with change trend of an anti-clockwise rotation of the faults from bottom up;(3) tectonic stress mechanisms had been transformed from extension during sedimentation of Quantou Formation-Mingshui Formation to strike-slip at the end period of the Mingshui Formation since formation of middle-shallow successions in the Daqing placanticline; and(4) the complicated faulting system in the study area formed from the process of the progressive deformation under the condition of maintaining a relatively steady principal direction of tectonic stress field. The new model for the evolution of the faults reasonably reveals the development rule and mechanism of the middle-shallow faulting system in the Songliao Basin, and will has guiding significance for further exploration and development of the study area.
引文
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