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河套盆地晚侏罗世逆冲构造及其油气地质意义

于波 李鹏 罗安湘 刘永涛 王维斌 李积轩 薛登 黄玺 毛黎光

地质科学2026,Vol.61Issue(4):1005-1011,7.
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地质科学2026,Vol.61Issue(4):1005-1011,7.DOI:10.12017/dzkx.2026.067

河套盆地晚侏罗世逆冲构造及其油气地质意义

Late Jurassic thrusting in the Hetao Basin and its petroleum geological significance

于波 1李鹏 2罗安湘 1刘永涛 2王维斌 1李积轩 3薛登 3黄玺 3毛黎光3

作者信息

  • 1. 中国石油天然气股份有限公司长庆油田分公司 西安 710018
  • 2. 中国石油集团东方地球物理勘探有限责任公司 河北涿州 072751
  • 3. 中国矿业大学(北京) 北京 100083
  • 折叠

摘要

Abstract

The Hetao Basin,located on the northwestern margin of the North China Craton,is a Cenozoic rift basin developed on cratonic basement.Based on drilling and seismic profile data,this study systematically compares and analyzes the basement structural characteristics of the Hetao Basin and the Ordos Basin.The results reveal that north of the Yellow River fault,the Lower Cretaceous to Cenozoic strata in the Hetao Basin unconformably overlie the Archean metamorphic basement,while south of the fault,the Ordos Basin preserves a complete succession of typical North China Craton cover sequences from the Changcheng System to the Cretaceous.Seismic profile analysis indicates that the Yellow River fault experienced south-directed thrusting during the Late Jurassic,leading to uplift and extensive erosion of the hanging wall rocks north of the fault,which resulted in the exhumation of the Archean basement to the surface.The widespread Late Jurassic thrust faulting along the northern margin of the North China Craton is likely associated with the closure of the Mongol-Okhotsk Ocean and subsequent continental collision events.

关键词

河套盆地/华北克拉通/鄂霍茨克洋/晚侏罗世/燕山运动

Key words

Hetao Basin/North China Craton/Okhotsk Ocean/Late Jurassic/Yanshanian orogeny

分类

天文与地球科学

引用本文复制引用

于波,李鹏,罗安湘,刘永涛,王维斌,李积轩,薛登,黄玺,毛黎光..河套盆地晚侏罗世逆冲构造及其油气地质意义[J].地质科学,2026,61(4):1005-1011,7.

基金项目

国家重点研发计划项目(编号:2022YFF0800200)、中国石油长庆油田分公司重大科技专项"鄂尔多斯盆地地震格架大剖面综合解释与基础地质研究"(编号:2023DZZ02)和"中央高校基本科研业务费"项目(编号:2023ZKPYDC08)资助 (编号:2022YFF0800200)

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