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塔里木盆地中生代沉积演化

程明 周露 史超群 娄洪 亢茜 吕惠贤

地质科学2026,Vol.61Issue(3):738-749,12.
地质科学2026,Vol.61Issue(3):738-749,12.DOI:10.12017/dzkx.2026.050

塔里木盆地中生代沉积演化

Mesozoic depositional evolution in the Tarim Basin

程明 1周露 2史超群 2娄洪 2亢茜 1吕惠贤1

作者信息

  • 1. 中国石油塔里木油田分公司勘探开发研究院 新疆库尔勒 841000||中国石油天然气集团有限公司超深层复杂油气藏勘探开发技术研发中心 新疆库尔勒 841000
  • 2. 中国石油塔里木油田分公司勘探开发研究院 新疆库尔勒 841000||中国石油天然气集团有限公司超深层复杂油气藏勘探开发技术研发中心 新疆库尔勒 841000||新疆超深油气重点实验室 新疆库尔勒 841000
  • 折叠

摘要

Abstract

In view of the analysis on Mesozoic sedimentary evolution in Tarim Basin,layer flattening technique was applied,and chronostratigraphy analysis of two seismic survey lines was completed,seismic cross sections were interpreted for each Mesozoic formation,and twelve residual time thickness maps were compiled for the first time.Based on these data,a preliminary sedimentary evolution analysis on the Mesozoic strata was conducted.Influenced by the Indosinian movement,the Mesozoic depocenter of the Tarim Basin shifted eastward from the Awati Sag during the Triassic.Subsequently,under the influence of the Early Yanshan movement,it continued to shift further eastward into the Manjiaer sag during the Jurassic.During the Cretaceous,the Manjiaer Sag was generally characterized by lacustrine transgression,under the influence of the Middle Yanshan movement,the deposition range expanded,the depocenter moved back to the northwest.Affected by the Indosinian and Yanshan movements,the Tadong uplift underwent rigid deformation,and fractures developed in the Jurassic strata.During the Early Cretaceous,the Tarim Basin as a whole experienced a broad and gentle extensional subsidence.In the Late Cretaceous,the basin underwent regional uplift and erosion due to the Late Yanshan movement.Mesozoic strata are characterized by fluvial-lacustrine sedimentation.

关键词

塔里木盆地/中生代/三叠系/侏罗系/白垩系/沉积演化

Key words

Tarim Basin/Mesozoic/Triassic/Jurassic/Cretaceous/Depositional evolution

分类

天文与地球科学

引用本文复制引用

程明,周露,史超群,娄洪,亢茜,吕惠贤..塔里木盆地中生代沉积演化[J].地质科学,2026,61(3):738-749,12.

基金项目

中国石油科技专项"超深层碎屑岩大中型油气田形成条件与有利区评价"(编号:2023ZZ14YJ01)和塔里木油田研发专项"塔里木盆地超深层碎屑岩沉积体系与成储机理研究"(编号:YF202502)资助 (编号:2023ZZ14YJ01)

地质科学

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