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准噶尔盆地西部地区主要不整合面形成演化与油气地质意义

WEI Xiaosong YAN Detian ZHENG Menglin TANG Yong ZHANG Lei XU Shiqi ILYHAMJAN Tuniyaz ZHANG Bao YUAN Duoen

地质学报2025,Vol.99Issue(12):4019-4037,19.
地质学报2025,Vol.99Issue(12):4019-4037,19.DOI:10.19762/j.cnki.dizhixuebao.2025246

准噶尔盆地西部地区主要不整合面形成演化与油气地质意义

The formation,evolution,and petroleum geological significance of major unconformities in the western region of the Junggar basin,China

WEI Xiaosong 1YAN Detian 2ZHENG Menglin 3TANG Yong 4ZHANG Lei 3XU Shiqi 5ILYHAMJAN Tuniyaz 5ZHANG Bao 6YUAN Duoen1

作者信息

  • 1. Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences(Wuhan),Wuhan,Hubei 430074,China
  • 2. Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences(Wuhan),Wuhan,Hubei 430074,China||Urumqi Geological Brigade,Bureau of Geology of Xinjiang Uygur Autonomous Region,Urumqi,Xinjiang 830000,China
  • 3. Exploration and Development Research Institute of PetroChina Xinjiang Oilfield Company,Karamay,Xinjiang 834000,China
  • 4. Exploration and Development Research Institute of PetroChina Xinjiang Oilfield Company,Karamay,Xinjiang 834000,China||Xinjiang Research Institute of Huairou Laboratory,Urumqi,Xinjiang 830000,China
  • 5. Urumqi Geological Brigade,Bureau of Geology of Xinjiang Uygur Autonomous Region,Urumqi,Xinjiang 830000,China
  • 6. Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences(Wuhan),Wuhan,Hubei 430074,China||Sinopec Jianghan Oilfield Exploration and Production Research Institute,Wuhan,Hubei 430070,China
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摘要

Abstract

Basedon regional 2D/3D seismic profiles of the Junggar basin,this study systematically investigates five major regional unconformities:the Permian/Carboniferous(P/C),Lower Triassic-Upper Permian/Middle-Lower Permian(T-P3/P2),Jurassic/Triassic(J/T),Cretaceous/Jurassic(K/J),and Paleogene/Cretaceous(E/K).By analyzing their contact relationships and seismic reflection characteristics,and denudation features,the spatial distribution and tectonic genesis of each unconformity are clarified.The results indicate:① Distinct Zonation:the P/C unconformity is developed in the western uplift zone,characterized by the truncation of Carboniferous volcanic rocks and overlying Permian onlap deposits.The T-P3/P2 unconformity is concentrated in the northwestern fault belt,exhibiting typical truncation-onlap characteristics.The J/T and K/J unconformities are distributed across the central uplift areas,dominated by a disconformity in the Luliang uplift,whereas the E/K unconformity has migrated to the northern and southern foreland belts.② Orogeny-controlled formation mechanisms:the P/C angular unconformity was triggered by the Late Paleozoic closure of the West Junggar Ocean(~300 Ma).During the Indosinian(~260 Ma),the remote effect of the Paleo-Tethys closure induced dextral strike-slip and thrusting along the Kebai fault zone,forming the localized T-P3/P2 unconformity.Subsequently,Yanshanian(200~145 Ma)intracontinental collisions led to the formation of the J/T and K/J unconformities.Finally,the Himalayan-stage(~50 Ma)India-Eurasia collision generated high-angle E/K unconformities along the basin margins.③ Triple control on hydrocarbon accumulation:unconformities influence hydrocarbon enrichment through three key mechanisms:reservoir improvement(e.g.,80~120 m of secondary porosity in the P/C weathering crust),hydrocarbon migration pathways(e.g.,lateral transport along J/T surfaces),and reservoir-seal assemblages(e.g.,the Baikouquan sandstone-mudstone configuration).This study provides a geological framework for exploring subtle hydrocarbon reservoirs in the Junggar basin.

关键词

准噶尔盆地/不整合面/构造演化/油气成藏/应力场迁移/盆山耦合

Key words

Junggar basin/unconformity/tectonic evolution/hydrocarbon accumulation/stress field migration/basin-mountain coupling

引用本文复制引用

WEI Xiaosong,YAN Detian,ZHENG Menglin,TANG Yong,ZHANG Lei,XU Shiqi,ILYHAMJAN Tuniyaz,ZHANG Bao,YUAN Duoen..准噶尔盆地西部地区主要不整合面形成演化与油气地质意义[J].地质学报,2025,99(12):4019-4037,19.

基金项目

本文为中国石油天然气股份有限公司"十四五"前瞻性基础性重大科技项目(编号2022DJ0108)资助的成果. (编号2022DJ0108)

地质学报

OA北大核心

0001-5717

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