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海南岛东寨港1605年地震陷落事件的地球化学证据
  • ISSN号:1001-7410
  • 期刊名称:第四纪研究
  • 时间:2012.1.1
  • 页码:1248-1255
  • 分类:P315.724[天文地球—地震学;天文地球—固体地球物理学;天文地球—地球物理学]
  • 作者机构:[1]南京大学地理与海洋科学学院海岸海洋科学系,海岸与海岛开发教育部重点实验室,南京210093, [2]中国科学院南海海洋研究所边缘海地质重点实验室,广州510301
  • 相关基金:国家自然科学基金项目(批准号:40676052和41071006)、江苏省高校优势学科项目和中国科学院边缘海重点实验室开放课题项目(批准号:NSGL0502)共同资助
  • 相关项目:江苏圆陀角附近潮滩近期快速淤涨的沉积记录与形成机理
作者: 张振克|
中文摘要:

1605年海南岛东寨港发生了重要的地震陷落事件,本文在东寨港采集了305cm长的柱状岩芯DX孔,对岩芯进行了粒度、年代学、地球化学元素的分析,发现地球化学元素在164cm附近有明显的突变,岩芯沉积物岩性特征与地球化学元素均反映了从陆相沉积向海相沉积的转变,对海南岛东寨港地震陷落事件有明显的沉积响应,岩芯沉积记录反映1605年东寨港地震沉陷的幅度至少2.0m。

英文摘要:

The Dongzhai Bay,located in the north-eastern part of the Hainan Island.The serious earthquake in the year of 1605 occurred at Qiongzhou(present Haikou City)in the region close to present Dongzhai Bay,which was the most extensive earthquake recorded in the historical documents in South China with the seismic magnitude of 7.5 and the intensity of 10 degrees.This historical earthquake resulted in the land subsidence and the formation of the Dongzhai Bay.According to the Ming Dynasty "Qiongzhou Government Document",a strong earthquake occurred on July 131605A.D.The ground sounds came from northeast like depressing thunder with vibrating and the local governmental halls,private houses mostly collapsed in Qiongzhou.In the town of Qiongzhou,the death number was about thousands people.In the coastal region large areas of land,villages sunk in to the sea.So the Dongzhai Bay is a very young bay related to the historical earthquake in the year of 1605.In the past decades,the Qiongzhou Earthquake in the year of 1605 was interested by the Chinese researchers. The serious earthquake in the year of 1605 occurred at Qiongshan was the most extensive earthquake recoded in the historical documents in South China with the seismic intensity of M7.5.It is an interesting research to study the sedimentary records of the earthquake subsidence in Dongzhai Bay,Hainan Island.Based on the analysis of the core samples,sedimentary characteristics and elements composition changes,the coastal sedimentary respond to the historical earthquake was presented and the analysis indicated the at least 2.0meters subsidence influenced by the earthquake in the western part of the Dongzhai Bay.The 305cm long DX Core at Daoxue Village(19°55.876'N, 110°35.806'E) was collected and sampling with the intervals of 2.5cm,sedimentary characteristics,grain seize and elements composition changes are obviously related to the earthquake.The coastal sedimentary respond to the historical earthquake was presented in this paper.In the column of the D

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期刊信息
  • 《第四纪研究》
  • 中国科技核心期刊
  • 主管单位:中国科学院
  • 主办单位:中国科学院地质与地球物理研究所 中国第四纪研究委员会
  • 主编:郭正堂
  • 地址:北京9825信箱
  • 邮编:100029
  • 邮箱:dsj@mail.igcas.ac.cn dsjs@mail.igcas.ac.cn
  • 电话:010-82998119
  • 国际标准刊号:ISSN:1001-7410
  • 国内统一刊号:ISSN:11-2708/P
  • 邮发代号:82-428
  • 获奖情况:
  • 1996年被国务院学位委员会地球物理及地质学科评议...,2001年入中国期刊方阵,2007年获中国科学院出版基金科技期刊排行榜三等奖
  • 国内外数据库收录:
  • 美国化学文摘(网络版),英国动物学记录,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:17826