首页|库车前陆冲断带构造分层变形特征

库车前陆冲断带构造分层变形特征

扫码查看
原文链接
  • NETL
  • NSTL
  • 万方数据
库车前陆冲断带地震资料信噪比低,具有多解性.利用高分辨率三维地震、钻井、油气分析化验等资料,对库车前陆冲断带地层组合进行系统描述,精细解释构造模型,深入剖析油气成藏体系,认为库车前陆冲断带发育古近系和新近系膏盐岩层及三叠系和侏罗系煤层2套滑脱层,具有分层滑脱、垂向叠置、多期变形的特征,浅层构造发育盖层滑脱褶皱,深层发育基底卷入式叠瓦状逆冲构造,膏盐岩层和煤层发生滑脱塑性变形,发育加里东运动期、海西运动晚期—印支运动期和燕山运动期—喜马拉雅运动期3期断裂,海西运动晚期—印支运动期构造控制中生界沉积,由北向南具有超覆减薄的特征.库车前陆冲断带分层构造变形控制油气分层运聚,煤层以上的油气主要来自侏罗系烃源岩,煤层之下的油气主要来自三叠系,三叠系烃源岩生烃量占60%,大量油气仍保存在煤层之下.
Layered Structural Deformation Characteristics of Kuqa Foreland Thrust Belt
The seismic data acquired from Kuqa foreland thrust belt is characterized by low signal-to-noise ratio and high interpretive am-biguity.By using high-resolution 3D seismic data,drilling and lab hydrocarbon analysis data,the stratigraphic assemblages of Kuqa fore-land thrust belt were systematically described,the structural model was detailedly interpreted,and the hydrocarbon accumulation system was deeply analyzed.It is found that the Kuqa foreland thrust belt develops two sets of detachment layers:Paleogene and Neogene gypsum-salt rocks,and Triassic and Jurassic coal measures,all of which feature stratified detachment,vertical stacking,and multiphase deforma-tion.Detachment folds in caprocks are found in the shallow structures,while basement-involved imbricate thrust structures are developed in deep strata.Detachment plastic deformation occured in the gypsum-salt and coal layers.Faulting occured in three phases including Cale-donian,late Hercynian-Indosinian,and Yanshanian-Himalayan.The late Hercynian-Indosinian tectonics controlled the Mesozoic sedi-mentation,showing a north-to-south onlap thinning feature.Layered structural deformation in the Kuqa foreland thrust belt governs the stratified accumulation and migration of hydrocarbons.Hydrocarbons in the strata above the coal seam predominantly originated from the Jurassic source rocks,whereas oil and gas in the strata below the coal seam mainly came from the Triassic source rocks which contributs 60%of the hydrocarbons.A substantial quantity of hydrocarbon remains trapped in the formation below the coal layer.

Kuqa foreland thrust beltcoal seamgypsum-salt layerdetachment layerlayered structural deformationstratified hydrocar-bon accumulation and migrationdeep oil and gas

徐振平、杨宪彰、能源、段云江、张文、胡建宁、张梦洋

展开 >

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

中国石油大学(北京)克拉玛依校区 石油学院,新疆 克拉玛依 834000

中国石油大学(北京)地球科学学院,北京 102499

库车前陆冲断带 煤层 膏盐岩层 滑脱层 构造分层变形 油气分层运聚 深层油气

国家自然科学基金国家重点研发项目

423620262019YFC0605505

2024

10.7657/XJPG20240501

新疆石油地质
新疆石油学会

新疆石油地质

CSTPCD北大核心
影响因子：0.985
ISSN：1001-3873
年,卷(期)：2024.45(5)