石油学报 ›› 1986, Vol. 7 ›› Issue (4): 25-30.DOI: 10.7623/syxb198604004

• 地质勘探 • 上一篇    下一篇

川东地区构造叠加作用

张月华   

  1. 四川石油勘探开发研究院
  • 收稿日期:1984-05-20 出版日期:1986-10-25 发布日期:2013-07-08

ANALYSIS OF STRUCTURAL OVERLAPPING IN EASTERN SICHUAN

Zhang Yuehua   

  1. The Sichuan Institute of Petroleum Exploration and Development
  • Received:1984-05-20 Online:1986-10-25 Published:2013-07-08

摘要: 本文主要分析了川东地区构造叠加现象、叠加变形顺序和时代、构造叠加过程、叠加构造类型与油气关系。认为川东地区复杂的构造面貌是由早、晚两期构造叠加形成,早期变形时代为晚白垩世晚期,由于太平洋板块的推挤,使区内基底断裂发生平移,形成北北东-北东向低缓的S形斜列构造,同时形成有规律分布的北东东向构造。晚期褶皱属喜山构造旋回,可能由于印度板块的推挤,在区内沿早期构造线追踪叠加,形成现今构造面貌,并同时形成近南北向的低潜构造。在油气勘探中,注意两期正向构造叠加形成的重叠型和交叉叠加型构造,特别是类似卧龙河这类盖层条件较好的重叠型构造。

Abstract: This paper mainly concerns the phenomena of structural overlapping, the time and order of overlapping deformation, the process of structural overlapping and the relationship between the types of overlapped structures and hydrocarbon accumulations in Eastern Sichuan. It holds that the complex structural features in Eastern Sichuan were formed by overlapping of two structural deformations. The first one took place in late upper Cretaceous and the second in Himalaya tectonic cycle. In exploring for oil and gas, attention should be payed to the types of overlapping and cross-overlapped structures which were formed by overlapping of two periods of positive structures, especialy to the overlapped structures similar to Wolong River structure which has very good cap rocks.