克拉美丽山与大井坳陷的构造关系&#x02014;&#x02014;兼论石炭纪构造-沉积格局

张磊; 何登发; 易泽军; 李涤

doi:10.11698/PED.2020.01.03

石油勘探与开发 >

2020 , Vol. 47 >Issue 1: 29 - 44

DOI: https://doi.org/10.11698/PED.2020.01.03

油气勘探

克拉美丽山与大井坳陷的构造关系——兼论石炭纪构造-沉积格局

张磊 ,
何登发 ,
易泽军 ,
李涤

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中国地质大学海相储集层演化与油气富集机理教育部重点实验室,北京100083

张磊（1988-）,男,湖南岳阳人,现为中国地质大学（北京）在读博士研究生,主要从事构造石油地质研究。地址：北京市海淀区学院路29号,中国地质大学（北京）海相储集层演化与油气富集机理教育部重点实验室,邮政编码：100083。E-mail: geozhanglei@163.com

收稿日期: 2019-04-17

网络出版日期: 2020-01-17

基金资助

国家自然科学基金青年项目（41702110）; 国家科技重大专项（2017ZX05001-001）; 国家重点研发计划（2017YFC0601405）

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Tectonic relationship between the Kelameili range and the Dajing depression: Insights into the Carboniferous tectonic-sedimentary framework

ZHANG Lei ,
HE Dengfa ,
YI Zejun ,
LI Di

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Key Laboratory of Marine Reservoir Evolution and Hydrocarbon Accumulation Mechanism, Ministry of Education, China University of Geosciences, Beijing 100083, China

Received date: 2019-04-17

Online published: 2020-01-17

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摘要

基于最新深钻井、地震剖面、年代学和野外露头等资料,利用轴面分析和平衡剖面等技术,精细解析克拉美丽山地质结构并分析其与大井坳陷的构造关系,对石炭纪不同时期的构造-沉积格局进行探讨。得到3个方面的认识：①研究区主要经历了早石炭世早期、石炭纪末期、中—晚二叠世、晚白垩世和古近纪5次构造挤压运动,早石炭世中—晚期、晚石炭世中—晚期和早二叠世3次伸展构造活动,其中在早二叠世末和中—晚白垩世分别发生了构造楔向南楔入;②克拉美丽山与大井坳陷的构造关系表现为早石炭世早期初次“盆”“山”耦合,之后经历了早石炭世中晚期—早二叠世一定程度的弱化,中二叠世的强耦合,后续的印支、燕山和喜马拉雅等运动都继承了这一“盆”“山”关系;③研究区在早石炭世早期为前陆盆地且发育滴水泉组烃源岩,早石炭世中—晚期发育多个北西向和北西西向半地堑式断陷盆地,形成松喀尔苏组火山岩储集层,早—晚石炭世之交进入裂陷后的拗陷盆地阶段,发育双井子组烃源岩,晚石炭世中—晚期发育断陷,形成上石炭统巴山组火山岩储集层,受石炭纪末、中二叠世的构造挤压作用,巴山组遭受大规模剥蚀,仅在山前坳陷带有部分残余。图11参57

关键词： 克拉美丽山; 大井坳陷; 盆山耦合; 石炭纪构造-沉积格局; 准噶尔东部地区; 准噶尔盆地

本文引用格式

张磊 , 何登发 , 易泽军 , 李涤 . 克拉美丽山与大井坳陷的构造关系——兼论石炭纪构造-沉积格局[J]. 石油勘探与开发, 2020 , 47(1) : 29 -44 . DOI: 10.11698/PED.2020.01.03

Abstract

Based on comprehensive analysis of typical outcrops, latest deep wells drilled and high resolution seismic profiles in the study area, we examined the geologic structure of the Kelameili range, and analyzed the structural relationship between the Kelameili range and the Dajing depression, and discussed the tectonic-sedimentary framework in different periods of Carboniferous by using axial surface analysis and balanced section techniques. Understandings in three aspects are achieved: (1) The study area experienced five stages of compressional tectonic movements, the Early Carboniferous, the Late Carboniferous, the Middle-Late Permian, Late Cretaceous and Paleogene, and three stages of extensional tectonic movements, the middle-late Early Carboniferous, the middle-late Late Carboniferous and Early Permian. At the end of the Early Permian and the Mid-Late Cretaceous, the tectonic wedges moved southward respectively. (2) The Kelameili range and Dajing depression had the first basin-range coupling during the early Early Carboniferous, basin-range decoupling in the following middle-late Early Carboniferous to the Early Permian, then basin-range strong recoupling in the Middle Permian, and the basin-range coupling had been inherited in the subsequent Indosinian, Yanshanian and Himalayan movements. (3) During the early Early Carboniferous, the study area was a foreland basin where the Dishuiquan Formation source rock developed; in mid-late Early Carboniferous, a series of NW- and NWW-trending half-garben fault basins developed, where the Songkaersu Formation volcanic reservoir formed. In late Early Carboniferous, the study area entered into depression basin stage after rifting, and the Shuangjingzi Formation source rock developed; in the mid-late Late Carboniferous, Batamayineshan fault basin emerged, and the Upper-Carboniferous volcanic reservoir was formed, affected by the tectonic compression during late Carboniferous and Mid-Permian, the Batamayineshan Formation suffered extensive erosion, and only partially remains in the piedmont depression zone.

Key words： Kelameili range; Dajing depression; basin-range coupling; Carboniferous tectonic-sedimentary framework; eastern Junggar Basin

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