石油学报 ›› 2026, Vol. 47 ›› Issue (3): 554-567.DOI: 10.7623/syxb202603004

• 地质勘探 • 上一篇    

塔里木盆地西南斜坡“开江—梁平海槽”式台内凹陷

管树巍1, 杨威1, 程明华2, 赵博2, 马培领2, 韩长伟2, 周慧1, 马德波1   

  1. 1. 中国石油勘探开发研究院 北京 100083;
    2. 中国石油集团东方地球物理勘探有限责任公司研究院塔里木物探研究院 新疆库尔勒 841000
  • 收稿日期:2025-08-22 修回日期:2025-09-08 发布日期:2026-04-09
  • 通讯作者: 管树巍,男,1970年6月生,2004年获浙江大学博士学位,现为中国石油勘探开发研究院高级工程师,主要从事含油气盆地构造分析工作。Email:guan@petrochina.com.cn
  • 作者简介:管树巍,男,1970年6月生,2004年获浙江大学博士学位,现为中国石油勘探开发研究院高级工程师,主要从事含油气盆地构造分析工作。Email:guan@petrochina.com.cn
  • 基金资助:
    国家自然科学基金重点项目(No.42330810)和中国石油天然气集团有限公司项目(2023ZZ02,2023ZZ16)资助。

A “Kaijiang-Liangping trough” type intra-platform sag in the southwestern slope of Tarim Basin

Guan Shuwei1, Yang Wei1, Cheng Minghua2, Zhao Bo2, Ma Peiling2, Han Changwei2, Zhou Hui1, Ma Debo1   

  1. 1. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China;
    2. Tarim Geophysical Research Institute, CNPC Bureau of Geophysical Prospecting Inc., Xinjiang Korla 841000, China
  • Received:2025-08-22 Revised:2025-09-08 Published:2026-04-09

摘要: 斜坡 是含油气盆地的主要构造单元,也是油气聚集的重要场所。塔西南斜坡占塔里木盆地近1/5的面积,但一直是勘探与研究的非重点地区。通过对比中国中西部4大盆地斜坡区的石炭系—二叠系构造背景、油气地质条件及勘探现状,指出油气主要聚集在源内以及与烃源岩同期的岩性储集体内,而斜坡边缘的晚期构造(如山前冲断带)并非主要聚集场所。区域构造与古地理研究表明,塔里木地块西南缘在石炭纪—早二叠世是一个向西倾斜的大陆边缘盆地,发育碎屑岩-碳酸盐岩交替主导的混合沉积体系,塔西南斜坡主体处于局限台地—潮坪环境。早石炭世以来持续的伸展裂陷作用,如古特提斯洋向北俯冲导致的弧后扩张,以及早二叠世地幔柱活动与大规模玄武岩喷发,使得塔西南斜坡发育类似"开江—梁平海槽"的台内凹陷。现有的研究数据证实,该台内凹陷呈近EW向展布,石炭系—下二叠统的最大充填厚度逾2 300 m,面积逾2×104km2。凹陷内部发育下石炭统卡拉沙依组优质烃源岩,其分布面积和厚度与四川盆地北斜坡"开江—梁平海槽"内的上二叠统龙潭组和大隆组烃源岩相当。塔西南斜坡的石炭系—下二叠统台内凹陷是一个现实的含油气系统,具有源内非常规和源外常规两种油气聚集类型,是塔里木盆地海相深层油气勘探的另 一个重要方向。

关键词: 台内凹陷, 开江—梁平海槽, 弧后扩张, 卡拉沙依组, 塔西南斜坡

Abstract: Slope belts are primary structural units in petroliferous basin, and key sites for oil and gas accumulation. The southwestern slope of Tarim Basin, occupying nearly one-fifth of its total area, has been a non-priority area for exploration and research. By comparing the Carboniferous-Permian tectonic setting, hydrocarbon geological conditions and exploration status in the slope areas of the four major basins in central and western China, it is pointed out that hydrocarbons in the slope area are mainly accumulated within the source rocks and in the contemporaneous lithologic reservoirs. Late-stage structures along the slope margin, such as piedmont thrust belts, are not the primary hydrocarbon accumulation zone. Regional tectonic and paleogeographic studies indicate that during the Carboniferous to Early Permian, the southwestern margin of Tarim block was a west-dipping continental margin basin, which developed a mixed sedimentary system alternately dominated by clastic rocks and carbonate rocks. The southwestern slope of Tarim Basin was largely dominated by the restricted platform and tidal flat environments. The continuous extensional rifting since the Early Carboniferous, such as the back-arc extension caused by the northward subduction of the Paleo-Tethys Ocean, as well as mantle plume activity and large-scale basalt eruption in the Early Permian, led to the development of the intra-platform sag analogous to the Kaijiang- Liangping trough on the southwestern slope of Tarim Basin. Existing research data demonstrate a predominant east-west trending structure in the intra-platform sag, and the Carboniferous to Lower Permian reservoirs exhibit the maximum sedimentary thickness exceeding 2 500 m, with an area of more than 20 000 km2. High-quality source rocks in sag are developed in the Lower Carboniferous Kalashayi Formation, with a distribution area and thickness comparable to those of the Upper Permian Longtan and Dalong formations within the Kaijiang-Liangping trough in the northern slope of Sichuan Basin. The Carboniferous to Lower Permian intra-platform sag is a realistic petroleum system with two types of hydrocarbon accumulation, i.e., in-source unconventional and extra-source conventional hydrocarbon accumulations, suggesting another important target area for deep marine oil and gas exploration in Tarim Basin.

Key words: i ntra-platform sag, Kaijiang-Liangping trough, back-arc extension, Kalashayi Formation, southwestern slope of Tarim Basin

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