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 HUAIYINXIANGSHUIKOU FAULT IN THE WATERS AROUND THE KAISHAN ISLAND USING MULTIPLE METHODS

作　　者：臧小豹[1] 薛怀友 戴俊成 

机构地区：[1]江苏省地质矿产调查研究所,江苏南京210043

出　　处：《安徽地质》2015年第2期83-86,共4页Geology of Anhui

基　　金：江苏省地勘基金;项目编号:2013255-1

摘　　要：淮阴—响水口断裂为江苏地层分区的重要界线,其陆域位置研究历来已久,但海域位置至今尚未明确。本次研究利用多方法手段,首次确定了淮阴-响水口断裂在南黄海海域的具体位置走向,并明确了开山岛地层归属。The Huaiyin-Xiangshuikou fault is a major borderline as a stratigraphic division in Jiangsu. It studied long for its extension on the land, but is so far unclear for its part in the marine area. With many and measures, this study first determined specific location and trending of the fault in southern Yellow and made clear the stratigraphic attribution of the Kaishan Island. has been methods Sea area

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 

分 类 号：P315.2[天文地球—地震学]