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现代地质 ›› 2014, Vol. 28 ›› Issue (6): 1260-1265.

• 构造地质学 • 上一篇    下一篇

塔里木盆地玉北地区玉东3断裂带构造转换特征分析

赵彬彬1,2,3,汤良杰1,2,余腾孝4,陈刚1,2,岳勇4,杨勇1,2,张旭光4,潘玉芳1,2   

  1. (1.中国石油大学(北京)油气资源与探测国家重点实验室,北京102249;
    2.中国石油大学(北京)盆地与油藏研究中心,北京102249; 3.新疆维吾尔自治区地震局,新疆 乌鲁木齐830011;
    4.中国石化 西北油田分公司,新疆 乌鲁木齐 830011)
  • 出版日期:2014-12-27 发布日期:2015-01-30
  • 作者简介:赵彬彬,女,硕士,1988年出生,构造地质学专业,主要从事含油气盆地构造研究工作。 Email: tszhaobinbin@126.com。

Transfer Zone Characteristics of the Yudong 3 Fault Zone in Yubei Area of the Tarim Basin

ZHAO Bin-bin1,2,3,TANG Liang-jie1, 2,YU Teng-xiao4,CHEN Gang 1, 2,YUE Yong4
YANG Yong1, 2,ZHANG Xu-guang4,PAN Yufang1, 2   

  1. (1.State Key Laboratory of Petroleum Resource and Prospecting,China University of Petroleum,Beijing102249,China;
    2.Basin & Reservoir Research Center,China University of Petroleum,Beijing102249,China;
    3.Earthquake Administration of Xinjiang Uygur Autonomous Region, Urumqi,Xinjiang830011,China;
    4.Northwest Oilfield Company,SINOPEC,Urumqi, Xinjiang830011,China)
  • Online:2014-12-27 Published:2015-01-30

摘要:

通过对塔里木盆地玉北地区最新的三维地震资料进行解释分析,运用断层的位移-距离分析方法,探讨了玉东3断裂带的转换带特征,并分析了转换带形成的三个阶段。玉北地区断裂发育,主要为北西走向。由北向南,玉东3断裂带从北东段到南西段断层倾向由SE向逐渐变为NW向,根据这种变化及其剖面组合关系,采用Morley对转换带的分类方案,确定在转换段内形成了聚敛叠覆型转换带。转换段的转换带传递了北东段断层和南西段断层的位移量,使玉东3断裂带的总位移量保持一致。该转换带的形成演化主要经历了孤立逆断层、转换带形成和转换带复杂化等三个阶段。

关键词: 玉北地区, 玉东3断裂带, 分段性, 转换带, 演化特征

Abstract:

 Based on the interpretation of the latest 3D seismic profiles, this study discussed the characteristic and evolution of the transfer zone in Yudong 3 fault belt in Tarim Basin according to the analysis of displacement-distance method. The Yubei area mainly consists of a number of faults striking northwest. From the northeast section to the southwest section, the direction of the main fault gradually changed from southeast to northwest. According to the combination and intersection relations of fault structures in this area, the transfer zone in transform section was interpreted as convergent-overlap type based on the classification of Morley. The transfer zone between the two sections has transferred their displacements and keeps the conservation of fault displacements in Yudong 3 fault zone. The evolution of this transfer zone can be divided into three stages, i.e. the formation of isolated reverse fault, formation of transfer-zone and complication of transfer zone.

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