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南海西南次海盆洋中脊分段特征

李细兵 吴振利 李家彪

海洋地质与第四纪地质2013,Vol.33Issue(3):101-107,7.
海洋地质与第四纪地质2013,Vol.33Issue(3):101-107,7.DOI:10.3724/SP.J.1140.2013.03101

南海西南次海盆洋中脊分段特征

THE PRELIMINARY STUDY OF SEGMENTATION OF THE MID-OCEAN RIDGE IN SOUTHWEST SUB-BASIN OF THE SOUTH CHINA SEA

李细兵 1吴振利 2李家彪3

作者信息

  • 1. 南京大学地球科学与工程学院,南京210093
  • 2. 江苏省地震局,南京210014
  • 3. 国家海洋局第二海洋研究所,杭州310012
  • 折叠

摘要

Abstract

According to the analysis of the geomorphology,gravity,magnetic data of the extinct mid-ocean ridge in southwest sub-basin of the South China Sea (SCS),a relict rifting center is found in the study area,of which the feature is similar to that of Atlantic mid-ocean ridge.Four transform faults are identified along the mid-ocean ridge in spatial location.Each of the transform faults shows distinct geophysical features compared with the others.The fourth one is specially discussed in details.It might be an important transition zone between the continental rifting and sea floor spreading,which implies a different crustal structure on both sides of the fault.

关键词

古洋中脊/分段性/转换断层/转换带/南海西南次海盆

Key words

extinct mid-ocean ridge/ segmentation/ transform fault/ transition zone/ southwest sub-basin of SCS

分类

海洋科学

引用本文复制引用

李细兵,吴振利,李家彪..南海西南次海盆洋中脊分段特征[J].海洋地质与第四纪地质,2013,33(3):101-107,7.

基金项目

国家自然科学基金项目(41106053) (41106053)

国家海洋局第二海洋研究所科研业务专项(JT201101) (JT201101)

海洋地质与第四纪地质

OA北大核心CSCDCSTPCD

0256-1492

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