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塔里木盆地麦盖提斜坡差异构造变形与油气聚集规律OA

Differential tectonic deformation and hydrocarbon accumulation patterns in the Maigaiti Slope of the Tarim Basin

中文摘要英文摘要

塔里木盆地麦盖提斜坡是重要的油气勘探区,但现有研究尚未明确斜坡内部复杂的差异变形过程及其对油气成藏的控制作用,制约了油气勘探开发的规模性突破.为此,基于二维、三维地震资料精细构造解析,划分了麦盖提斜坡三级构造单元,重新厘定了斜坡内部构造分区;进一步系统梳理了不同三级构造单元的断裂特征差异,并对麦盖提斜坡东西部的差异构造变形、演化过程与成因机制进行了分析,探讨了构造对油气聚集的控制作用.研究结果表明:①麦盖提斜坡可划分为巴什托北低缓褶皱带、巴岳鼻凸带、玉西鼻凸带和玉东—和田断褶带 4 个三级构造单元,"东西分区"特征显著;②西部为海西晚期麦西古隆起翼部大型鼻凸构造,北侧巴什托北低缓褶皱带以近东西向逆冲-走滑断裂为主,南侧巴岳鼻凸带发育北西向和北东向两组高陡直立走滑断裂;③中部玉西鼻凸带由和田古隆起在喜马拉雅期掀斜形成,主要发育以盐下为主的高陡直立走滑断裂;④东部玉东—和田断褶带发育加里东期前陆前隆带的多排冲断褶皱带.结论认为,差异构造变形决定了麦盖提斜坡不同构造单元成藏条件与勘探潜力,巴岳鼻凸带和玉西鼻凸带是最有利的油气勘探区带.

The Maigaiti Slope in the Tarim Basin is an important petroleum exploration area.However,the complex differential tectonic deformation within the Maigaiti Slope and its controlling effects on hydrocarbon accumulation remain inadequately understood,which restricts major breakthroughs in oil and gas exploration and development.Based on the detailed structure interpretation of 2D and 3D seismic data,this paper identifies the third-order structural units within the Maigaiti Slope,and revises the division of its structural zones.The differences in the fracture characteristics among these third-order structural units are systematically reviewed.Furthermore,the differential tectonic deformation,evolutionary processes and formation mechanisms in the western and eastern Maigaiti Slope are analyzed,and the structural controls on hydrocarbon accumulation are discussed.The following results are obtained.First,the Maigaiti Slope can be divided into four third-order structural units,namely the North Bashituo Gentle Fold Belt,the Ba-Yue Structural Nose,the Yuxi Structural Nose,and the Yudong-Hotan Fault-Fold Belt.It exhibits a pronounced east-west structural zonation.Second,the western Maigaiti Slope is characterized by a large structural nose developed on the flank of the Late Hercynian Maixi Paleo-uplift,where the North Bashituo Gentle Fold Belt is dominated by nearly E-W-trending thrust-strike&slip faults on the north and the Ba-Yue Structural Nose by steep NW-and NE-trending strike-slip faults on the south.Third,the central Yuxi Structural Nose was formed by Himalayan inversion of the Hotan Paleo-uplift and is dominated by steep strike-slip faults developed predominantly within the sub-salt succession.Fourth,the eastern Yudong-Hotan Fault-Fold Belt is dominated by multiple thrust-fold belts developed within the Caledonian forebulge.In conclusion,differential tectonic deformation determines the hydrocarbon accumulation conditions and exploration potential of different structural units in the Maigaiti Slope,and the Ba-Yue and Yuxi structural noses represent the most prospective exploration targets.

潘磊;张煜颖;何志勇;贺鸿冰;邱华标;王嘉宁

中国石化勘探分公司中国石化勘探分公司中国石化勘探分公司中国石化勘探分公司长江大学地球科学学院长江大学地球科学学院

能源科技

油气聚集差异构造变形构造解析麦盖提斜坡塔西南塔里木盆地巴岳鼻凸带玉西鼻凸带

Hydrocarbon accumulationDifferential tectonic deformationStructural analysisMaigaiti SlopeSouthwestern TarimTarim BasinBa-Yue structural noseYuxi structural nose

《天然气工业》 2026 (8)

32-45,14

中国石油化工股份有限公司科技部项目"塔西南地区油气富集主控因素与目标评价"(编号:P25147).

10.3787/j.issn.1000-0976.2026.08.003

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