石油与天然气地质 ›› 2015, Vol. 36 ›› Issue (4): 563-572.doi: 10.11743/ogg20150405

• 油气地质 • 上一篇    下一篇

塔里木盆地和田河气田玛扎塔格滑脱背斜构造特征

杨庚1,2, 李伟1,2, 陈竹新1,2, 石昕1,2, 雷永良1,2, 王晓波1,2   

  1. 1. 中国石油 勘探开发研究院, 北京, 10083;
    2. 提高石油采收率国家重点实验室, 北京, 10083
  • 收稿日期:2014-02-28 修回日期:2014-12-31 出版日期:2015-08-08 发布日期:2015-08-28
  • 第一作者简介:杨庚(1965—),男,博士、高级工程师,构造地质与盆地构造研究。E-mail:yanggeng@petrochina.com.cn。
  • 基金项目:
    国家科技重大专项(2011ZX05003-002);中石油股份公司科技专项(2014B-0407)。

Mazatage detachment anticline in Hetianhe gas field, Tarim Basin, western China

Yang Geng1,2, Li Wei1,2, Chen Zhuxin1,2, Shi Xin1,2, Lei Yongliang1,2, Wang Xiaobo1,2   

  1. 1. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China;
    2. State Key Laboratory of Enhanced Oil Recovery, Beijing 100083, China
  • Received:2014-02-28 Revised:2014-12-31 Online:2015-08-08 Published:2015-08-28

摘要: 塔里木盆地巴楚隆起南侧的和田河气田是在玛扎塔格构造上发现的典型背斜型气藏。由于该区钻井主要集中在构造核部,钻井深度相对较浅,而构造两翼的地震资料品质较差,因而对该构造出现了多种解释结果。本文依据钻井资料标定,应用断层相关褶皱理论,对该区二维地震剖面测网重新进行详细构造解释。结果表明,玛扎塔格构造主要构造样式为以中寒武统膏岩为滑脱面的滑脱背斜,玛4井东构造样式则为断层扩展褶皱,表明玛4井东存在近南北走向的横向走滑断层,并在地震剖面上得到证实。地震解释结果也证实了玛扎塔格构造西北侧发育的古董山逆冲断层向南东方向延伸进入和田河气田。滑脱褶皱背斜南北两翼发育的中新世-上新世生长地层和第四系角度不整合,表明该构造主要形成时期为中新世—上新世,而且第四纪该构造又重新活动。

关键词: 逆冲断层, 走滑断层, 滑脱背斜, 和田河气田, 塔里木盆地

Abstract: The Hetianhe gas field is one of the typical anticline gas reservoirs found in Mazatage structural belt of southern Bachu uplift in Tarim Basin.Previous exploration drilling is focused on core of the structure and the depths of exploratory wells are relatively shallow.Moreover, the quality of seismic data acquired on the flanks is poor.Therefore, structural interpretation was high in uncertainty.This paper tried to reinterpret the 2D seismic data based on calibration with drilling data and application of faulting-related fold theory.The result shows that the Mazatage structure is dominated by detachment anticline with the Middle Cambrian gypsum as detachment surface, while the part in the east of well Ma-4 in the structure is a fault-propagation fold, indicating the existence of a near NS-trending transverse strike-slip fault(seismic profile also revealed the same conclusion).Seismic interpretation also indicates that a thrust fault named Gudongshan deve-loped on the northwest flank of the structure extends into the Hetianhe gas field.The Miocene-Pliocene growth strata and Quaternary angular unconformity developed on the south and north flanks in the detached anticline show that the structure was probably formed during the Miocene-Pliocene period and reactivated during the Quaternary.

Key words: thrust fault, strike-slip fault, detached anticline, Hetianhe gas field, Tarim Basin

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