两期裂陷控制着地壳减薄和盆地演化——来自南海西北琼东南盆地南部的启示

IF 2.8 2区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Basin Research Pub Date : 2025-04-25 DOI:10.1111/bre.70030
Jingyuan Yu, Dianjun Tong, Chen Hu, Yancheng Xu, Jianye Ren
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引用次数: 0

摘要

在断陷边缘或断陷盆地,由于断裂体系的多期发育,盆地构造往往较为复杂。由于我们只能看到盆地演化的结果,因此很难判断早期断层活动对后期的影响。本文以琼东南盆地南部为例进行了研究,早期阶段的影响可以清晰地识别出来。利用新获得的高分辨率三维地震资料,分析了研究区新生代以来的构造原型和时间演化。根据断层活动和走向特征,确定了FS1、FS2和FS3 3个断层系统。观测结果表明,始新世末期应力场发生旋转,将整个裂谷作用划分为两个阶段。FS1发育于裂谷ⅰ期(42.5 ~ 33.9 Ma)北西—东西伸展期,为典型的基底型构造;FS2和FS3发育于裂谷ⅱ期(33.9 ~ 23.03 Ma)北南—南伸展期。FS1断裂或被FS2和FS3断裂横切成锯齿状平面几何,或在整个裂陷期成为寿命较长的活动断裂,导致应变局部化,地壳极度变薄。并可与南海北缘具有相同区域构造演化史的邻近盆地进行对比。长寿命的NE-SW向断裂导致研究区沉降史、盆地构造和地壳厚度沿走向发生显著变化,表明裂谷ⅰ期发育的断裂对裂谷ⅱ期盆地演化起着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Two Stages of Rifting Control the Crust Thinning and Basin Evolution: Insights From the Southern Qiongdongnan Basin, NW South China Sea

Two Stages of Rifting Control the Crust Thinning and Basin Evolution: Insights From the Southern Qiongdongnan Basin, NW South China Sea

In rifted margins or rifted basins, the structure of the basin is often complex due to the multistage development of fault systems. As we can only see the result of the basin evolution, it is difficult to judge the influence of early fault activity on the later stages. Here, we present a case study from the southern part of Qiongdongnan Basin (QDNB) where the influence of the early stage can be clearly recognised. Using newly acquired high-resolution 3D seismic datasets, we analyse the prototype and temporal evolution of the study area since the Cenozoic. Three fault systems (FS1, FS2 and FS3) were identified according to fault activities and fault strike. Observation results show a rotation of the stress field at the end of the Eocene, dividing the whole rifting into two stages. FS1 initiated in NW-SE extension at rift stage I (42.5–33.9 Ma), showing a typical basement-involved structure while FS2 and FS3 developed in N-S extension at rift stage II (33.9–23.03 Ma). The faults in FS1 were either crosscut to form a zigzag plane geometry by FS2 and FS3 faults, or became long-lived active faults throughout the rifting period, resulting in a localisation of strain and extremely thinning of the crust. It can also be compared with adjacent basins which have undergone the same regional tectonic evolution history at the northern margin of the South China Sea. The long-lived NE–SW trending faults cause significant variation in the subsidence history, basin structure, and crust thickness along strike in the study area, indicating that faults developed in rift stage I play a significant role in basin evolution at rift stage II.

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来源期刊
Basin Research
Basin Research 地学-地球科学综合
CiteScore
7.00
自引率
9.40%
发文量
88
审稿时长
>12 weeks
期刊介绍: Basin Research is an international journal which aims to publish original, high impact research papers on sedimentary basin systems. We view integrated, interdisciplinary research as being essential for the advancement of the subject area; therefore, we do not seek manuscripts focused purely on sedimentology, structural geology, or geophysics that have a natural home in specialist journals. Rather, we seek manuscripts that treat sedimentary basins as multi-component systems that require a multi-faceted approach to advance our understanding of their development. During deposition and subsidence we are concerned with large-scale geodynamic processes, heat flow, fluid flow, strain distribution, seismic and sequence stratigraphy, modelling, burial and inversion histories. In addition, we view the development of the source area, in terms of drainage networks, climate, erosion, denudation and sediment routing systems as vital to sedimentary basin systems. The underpinning requirement is that a contribution should be of interest to earth scientists of more than one discipline.
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