石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (1): 118-131.doi: 10.11743/ogg20220110
罗彩明1(), 梁鑫鑫2,3, 黄少英1, 能源2,3, 张玮1, 陈石2,3(), 曹淑娟1
收稿日期:
2020-12-11
修回日期:
2021-12-03
出版日期:
2022-02-01
发布日期:
2022-01-28
通讯作者:
陈石
E-mail:luocm?tlm@petrochina.com;chenshi4714@163.com
作者简介:
罗彩明(1980—),男,硕士、高级工程师,新区新领域风险勘探。E?mail: 基金资助:
Caiming Luo1(), Xinxin Liang2,3, Shaoying Huang1, Yuan Neng2,3, Wei Zhang1, Shi Chen2,3(), Shujuan Cao1
Received:
2020-12-11
Revised:
2021-12-03
Online:
2022-02-01
Published:
2022-01-28
Contact:
Shi Chen
E-mail:luocm?tlm@petrochina.com;chenshi4714@163.com
摘要:
塔中隆起位于塔里木盆地中央隆起带中部,为塔里木盆地油气勘探的重点区块之一。以塔中隆起高品质三维地震资料精细解释为基础,开展塔中隆起走滑断裂的剖面和平面几何学特征、断裂的活动期次和断裂形成机制研究。地震资料显示塔中走滑断裂于石炭纪之前定型,少数走滑断裂的活动持续到了石炭纪之后,断穿基底到志留系和泥盆系,断面直立,但是在不同层位断层的几何特征存在明显差异性,主要分为3层结构:深层中、下寒武统断裂平面上呈线性展布,中、下寒武统在断裂两侧上拱;深部断裂向上继续切穿上寒武统和奥陶系,并在碳酸盐岩顶面发育许多分支断裂,剖面上表现为正花状构造,平面上组合为斜列断裂;浅层走滑断裂发育在上奥陶统-志留系和泥盆系内,剖面上常以负花状构造样式出现,平面上表现为该层特有的北西向雁列断层。这3层断裂在垂向上叠置,形成复杂的空间形态,将塔中隆起走滑断裂的演化阶段划分为3期:中寒武世塔中地区存在构造反转事件,在压扭应力作用下发育规模较小的走滑断裂;晚奥陶世走滑断裂复活,形成正花状构造;志留纪—泥盆纪走滑断裂持续活动。塔中隆起走滑断裂的形成受周缘构造环境控制,在中寒武世局部压扭应力、晚奥陶世压扭环境和志留纪—泥盆纪的压扭环境下形成演化。
中图分类号:
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