渤海湾西岸全新世地层的分段与划组
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  • 英文篇名:Segmentation and grouping for the Holocence epoch strata in the west coast of Bohai Gulf
  • 作者:岳军 ; Dong ; Yue ; 赵希涛 ; 张宝华 ; 牟林 ; 韩芳 ; 王国明 ; 赵长荣 ; 张百鸣 ; 肖国强 ; 李建芬
  • 英文作者:Yue Jun~(1,2,3) Dong Yue~4 Zhao Xitao~5 Zhang Baohua~(1,3) Mu Lin~6 Han Fang~(1,3) Wang Guoming~2 Zhao Changrong~2 Zhang Baiming~7 Xiao Guoqiang~2 Li Jianfen~2 (1.Tianjin Marine Geology Exploration Center,Tianjin 300170;2.Tianjin Institute of Geology and Mineral Resources,CGS, Tianjin 300170;3.Geological Research Institute of North China Geological Exploration Bureau,Tianjin 300170; 4.University of Texas at San Antonio,Texas 78249-1644 USA;5.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029;6.Institute of Marine Science and Technology Information,Stale Oceanic Administration People's Republic of China,Tianjin 300160;7.Tianjin Geology and Mineral Bureau,Tianjin 300752)
  • 关键词:渤海湾西岸 ; 全新统 ; 地层层型剖面 ; 分段与划组
  • 英文关键词:West coast of Bohai Gulf;;Stratotype section of the Holocence epoch strata;;Segmentation and grouping
  • 中文刊名:DZKX
  • 英文刊名:Chinese Journal of Geology(Scientia Geologica Sinica)
  • 机构:天津市海洋地质勘查中心;国土资源部天津地质矿产研究所;天津华北地质勘查局地质研究所;University f Texas at San Antonio Texas 78249-1644 USA;中国科学院地质与地球物理研究所;国家海洋信息中心;天津市地质矿产勘查开发局;
  • 出版日期:2012-04-15
  • 出版单位:地质科学
  • 年:2012
  • 期:v.47
  • 基金:国家自然科学基金项目(编号:40940025,41006002);; 天津市自然科学基金项目(编号:07ZCGYSF02400与09JCYBJC07400);; 国家重点基础研究发展计划“973”项目(编号:2007CB411807);; 国家海洋局海洋大气—化学与全球变化重点实验室开放基金项目(编号:GCMAC0806)资助
  • 语种:中文;
  • 页:DZKX201202021
  • 页数:18
  • CN:02
  • ISSN:11-1937/P
  • 分类号:268-285
摘要
本文以岩性地层、气候地层(CaCO_3含量、古温度和Rb/Sr比值等)、年代地层、沉积化学地层和生物组合地层等资料为基础,根据地层规范以及建组要求将渤海湾西岸全新世地层划分为3个组:独流镇组(Qh_3dl)、大黄洼组(Qh_2dh)和西翟庄组(Qh_1xz)。其地层埋深界线及测年界线分别为:晚全新世独流镇组(Qh_3dl)与中全新世大黄洼组(Qh_2dh)的分组埋深界线为3.70 m,~(14)C年龄界线大致为2 820±80 a B.P.~2 390±60 a B.P.左右;中全新世大黄洼组(Qh_2dh)与早全新世西翟庄组(Qh_1xz)的分组埋深界线为14.10 m,~(14)C年龄界线大致为7 800±120 a B.P.~8 650±85 a B.P.左右;早全新世西翟庄组(Qh_1xz)与晚更新世塘沽组(QP_3tg)的分组埋深界线为18.70 m,测年~(14)C年龄界线大致为9 405±120 a B.P.~10 300±790 a B.P.左右。根据沉积地球化学环境指标(CaCO_3含量、古温度和Rb/Sr比值等)划分出第Ⅰ气候冷段~第Ⅴ气候冷段;根据C_(org)/P_2O_5、Fe~2/Fe~3等含量曲线综合分析划出第Ⅰ·还原带~第Ⅴ·还原带。综合分析显示:气候冷期时往往处于还原环境,与此同时,海平面则呈波动下降趋势。
        Based on the projects of "Comprehensive Geological Survey in Ninghe County,Tianjin", "Comprehensive Geological Survey in Jinghai County,Tianjin" and "Qilihai Geological Park", a few drilling holes are setted out in this area,take ZK01-ZK09 holes,BHN10 hole and BJM18 hole,SQ01-SQ29 holes and TK01-TK09 holes for example,the stratotype section of the Holocence epoch strata in the west coast of Bohai Gulf are segmented and divided into groups. According to stratigraphic code and grouping requirement,combing the data of lithologic stratigraphy,chronostratigraphy,chemistry strate and biological assemblages strate,the author divided the stratotype section of the holocence epoch strata into three groups:Duliuzhen group, Dahuangwa group,Xizhaizhuang group.The segmentation boundary between upper Holocence Duliuzhen group profiles and middle Holocence Dahuangwa group profiles are from 5.10 m to 5.25 m;the segmentation boundary between middle Holocence Dahuangwa group profiles and lower Holocence Xizhaizhuang group profiles are from 13.80 m to 14.10 m;the segementation boundary between lower Holocence Xizhaizhuang group profiles and lower Pleistoncene Tanggu group profiles are from 18.48 m to 18.70 m.The division ofⅠ~Ⅴcold climate section is accordance with the chemical environment related indexes,for example,the content of CaCO_3, pollen paleotemperature and the retio of Rb/Sr.The division ofⅠ·~Ⅴ·oxidation-reduction zone is accordance with the comprehensive analysis for the concentration curve of C_(org) /P_2O_5、Fe~(2+) /Fe~(3+).
引文
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