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南海北部深水区新生代盆地三层结构及其构造演化

能源 吴景富 漆家福 张功成 何玉平 陈玮常

地质学报2013,Vol.87Issue(3):403-414,12.
地质学报2013,Vol.87Issue(3):403-414,12.

南海北部深水区新生代盆地三层结构及其构造演化

Three Structural Layers and Its Evolution of Cenozoic Basins in Deep Water Area of Northern Margin, South China Sea

能源 1吴景富 2漆家福 3张功成 1何玉平 3陈玮常3

作者信息

  • 1. 中国石油大学(北京)油气资源与探测国家重点实验室,北京,102249
  • 2. 中国石油塔里木油田公司勘探开发研究院,新疆库尔勒,841000
  • 3. 中海石油研究总院勘探院,北京,100027
  • 折叠

摘要

Abstract

Continental margins, which locate in the continental crusts and oceanic crusts, record the processes of the continental breakup and the ocean opening. It is important for the research on the geodynamics. The Cenozoic basins in deep water of northern margin of South China Sea located on the continental margin. The Cenozoic basin can be divided into three structural layers. They are rift layer, post-rift depression layer and post-rift subsidence of ocean basin layer. Rift basin layer performed as a series of graben and half graben. The character of post-rift depression layer is thick in the middle and thin on both side which looks like a disk. The thickness of post-rift subsidence of ocean basin layer changed greatly, it thick on the continental slope and thin on the ocean basin which showed the character as a "flexing basin". The basin in deep water of northern margin South China Sea has experienced three evolution stages and showed the different geodynamic mechanisms. Influenced by the upwelling of the mantle, the basin mainly performed as horizontal extensional and formed the extensional structural styles in rift stage. In post rift stage, the basin subsided widely. In the third stage, the basin bended towards the South China Sea which controlled by the subsidence of ocean basin. The structural framework of continental shelf - continental slope - ocean basin is formed in the stage of ocean basin subsided. The activity difference of mantle material which under the basin of northern margin and the ocean basin is the main influence factors of the geodynamics.

关键词

南海北部/深水区/盆地结构/构造样式/构造演化

Key words

northern margin of South China Sea/ deep water area/ basin structural/ structural styles/ tectonic evolution

引用本文复制引用

能源,吴景富,漆家福,张功成,何玉平,陈玮常..南海北部深水区新生代盆地三层结构及其构造演化[J].地质学报,2013,87(3):403-414,12.

基金项目

本文为国家科技重大专项课题(编号2008ZX05025-02-01)、中国石油大学教育基金会"王涛英才奖学金"共同资助的成果. (编号2008ZX05025-02-01)

地质学报

OA北大核心CSCDCSTPCD

0001-5717

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