新疆石油地质 ›› 2021, Vol. 42 ›› Issue (6): 656-665.doi: 10.7657/XJPG20210602
收稿日期:
2021-01-08
修回日期:
2021-06-07
出版日期:
2021-12-01
发布日期:
2021-11-30
作者简介:
杨庚(1965-),男,山西大同人,高级工程师,博士,盆地构造分析与石油地质,(Tel)010-83592604(E-mail) 基金资助:
YANG Geng(), CHEN Zhuxin, WANG Xiaobo
Received:
2021-01-08
Revised:
2021-06-07
Online:
2021-12-01
Published:
2021-11-30
摘要:
塔里木盆地西南缘位于西昆仑山前,发育多个逆冲构造带,并发现了多个油气田。应用断层相关褶皱理论,根据钻井和二维地震资料,对塔西南山前的英吉莎背斜构造进行了精细的构造解释,发现了位于中新统安居安组泥岩和膏泥岩中的浅层滑脱层,浅层发育简单的被改造的断层弯曲褶皱,据此提出英吉莎背斜由浅层、中—深层和深层3个构造层垂向叠合而成。中—深层发育楔形构造,为多个逆冲断层的叠瓦状构造,深层为简单的楔形构造。根据生长地层及构造变形样式,浅层构造形成最早,其后为中—深层构造,深层构造形成最晚。总之,由西昆仑山向塔里木盆地呈现多期幕式逆冲,塔西南逆冲构造具多期幕式活动,不同时期发育的构造在垂向上叠加,形成现今的构造样式。
中图分类号:
杨庚, 陈竹新, 王晓波. 塔西南逆冲带前缘英吉莎背斜的多期变形[J]. 新疆石油地质, 2021, 42(6): 656-665.
YANG Geng, CHEN Zhuxin, WANG Xiaobo. Multistage Deformation of Yingjisha Anticline in the Front of Southwestern Tarim Thrust Belt, Northwestern China[J]. Xinjiang Petroleum Geology, 2021, 42(6): 656-665.
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