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基于多方法手段的开山岛海域淮阴-响水口断裂走向研究

臧小豹 薛怀友 戴俊成

安徽地质Issue(2):83-86,4.
安徽地质Issue(2):83-86,4.

基于多方法手段的开山岛海域淮阴-响水口断裂走向研究

Study on the trend of the huAiyin-XiAnGShuikou fAult in the wAterS Around the kAiShAn iSlAnd uSinG multiple methodS

臧小豹 1薛怀友 1戴俊成1

作者信息

  • 1. 江苏省地质矿产调查研究所,江苏南京.210043
  • 折叠

摘要

Abstract

The Huaiyin-Xiangshuikou fault is a major borderline as a stratigraphic division in Jiangsu. It has been studied long for its extension on the land, but is so far unclear for its part in the marine area. With many methods and measures, this study first determined specific location and trending of the fault in southern Yellow Sea area and made clear the stratigraphic attribution of the Kaishan Island.

关键词

断裂/淮阴-响水口断裂/苏北-南黄海断陷盆地/下扬子地台

Key words

fault/Huaiyin-Xiangshuikou fault/Subei-Southern Yellow Sea rifted basin/Lower Yangtze platform

分类

天文与地球科学

引用本文复制引用

臧小豹,薛怀友,戴俊成..基于多方法手段的开山岛海域淮阴-响水口断裂走向研究[J].安徽地质,2015,(2):83-86,4.

基金项目

江苏省地勘基金,项目编号2013255-1 ()

安徽地质

1005-6157

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