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构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例

构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_wanfang_journals_hydzydsjdz202105013

构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例

About this item

Full title

构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例

Publisher

Beijing: Marine Geology and Quaternary Geology

Journal title

Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ, 2021-01, Vol.41 (5), p.139-150

Language

Chinese

Formats

Publication information

Publisher

Beijing: Marine Geology and Quaternary Geology

More information

Scope and Contents

Contents

以构造变形为核心的内动力过程和以沉积“源–汇”过程为核心的外动力过程,如何动态塑造盆地精细地貌景观,是油气精准勘探必须突破的关键技术。本研究以南海北部陆缘珠江口盆地的阳江凹陷为例,试图探索NW向阳江–一统暗沙深大断裂带对周缘新生代沉降中心分布的控制作用。为此,本文采用Badlands沉积数值模拟方法,定量分析阳江–一统暗沙断裂带的运动学特征,模拟阳江凹陷新生代地层构造-沉积耦合过程。模拟结果显示,阳江–一统暗沙断裂带在始新世末期是一条左行走滑断裂带,其走滑过程主要可分为两个阶段。其中,在早期慢走滑阶段,走滑位移量约800 m,沿断裂带走滑方向,恩平19洼的沉降中心发生迁移;在后期快走滑阶段,走滑位移量约1200 m,模拟剖面可识别出明显的花状构造,恩平19洼的沉降中心加速向北迁移,并发生逆时...

Alternative Titles

Full title

构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_wanfang_journals_hydzydsjdz202105013

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_wanfang_journals_hydzydsjdz202105013

Other Identifiers

ISSN

0256-1492

DOI

10.16562/j.cnki.0256-1492.2021040601

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