唐佐其,刘凌云,谯文浪,陈武,华兴,吕留彦,马义波.黔东北寒武系牛蹄塘组沉积学特征及沉积环境演化[J].贵州地质,2019,36(1):61-68
黔东北寒武系牛蹄塘组沉积学特征及沉积环境演化
Sedimentology Characteristics and Sedimentary Environment Evolution in Niutitang Formation of Cambrianin Northeast Guizhou
投稿时间:2018-10-15  
DOI:
中文关键词:  黔东北  牛蹄塘组  微量元素  沉积环境演化
英文关键词:Northeast guizhou  Niutitang formation  Traceelement  Sedimentary environment evolution
基金项目:中国矿产地质志项目(DD20160346、DD20190379),贵州省地矿局科研项目(黔地矿科合[2012]16号、黔地矿科合[2017]29号)。
作者单位
唐佐其 贵州省地质调查院、贵州省地质物探开发应用工程技术研究中心、贵州省地质调查院院士工作站贵州贵阳550081 
刘凌云 贵州省地质调查院、贵州省地质物探开发应用工程技术研究中心、贵州省地质调查院院士工作站贵州贵阳550081 
谯文浪 贵州省地矿局102地质大队贵州遵义563000 
陈武 贵州省地质调查院、贵州省地质物探开发应用工程技术研究中心、贵州省地质调查院院士工作站贵州贵阳550081 
华兴 贵州省地质调查院、贵州省地质物探开发应用工程技术研究中心、贵州省地质调查院院士工作站贵州贵阳550081 
吕留彦 贵州省地质调查院、贵州省地质物探开发应用工程技术研究中心、贵州省地质调查院院士工作站贵州贵阳550081 
马义波 贵州省地质调查院、贵州省地质物探开发应用工程技术研究中心、贵州省地质调查院院士工作站贵州贵阳550081 
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中文摘要:
      通过对黔东北松桃-江口地区寒武系牛蹄塘组调查研究及系统的样品控制,以岩石学、层序地层学、微量元素地球化学为技术手段,研究发现该组地层岩石主要为富含炭质细碎屑岩组合,沉积构造丰富,识别出该地层组为完整的三级层序,自下而上可进一步划分为盆地-大陆斜坡-深水陆棚相沉积。微量元素总体上富亲铜、亲铁元素,贫亲石元素;以V、Ni、Mo、Re、As、Cd、U元素丰度及U/Th、δU、V/(V+Ni)、V/Cr、Ni/Co比值指标证实研究区牛蹄塘组中下部沉积条件均位于氧化界以下,属于贫氧-厌氧还原环境,为区域上V、Mo等元素的超常富集提供必要条件,至本组上部为贫氧-弱氧化环境,划分出Ⅶ个氧化还原幕次,细化了研究区牛蹄塘组沉积环境条件及其演化特征。
英文摘要:
      Field investigation and systematic sampling of the Niutitang formation of the Cambrian system in Songtao-Jiangkou area of northeast Guizhou were conducted,Petrologic sequence stratigraphy and trace element geochemistry are the technical means,It is found that the stratigraphic rocks in this group are mainly composed of carbonaceous fine clastic rocks,The formation is identified as a complete three-level Sequence,From bottom to top, it can be divided into basin slope, continental slope and deep water shelf facies。The trace elements are rich in copper and iron, and poor in stone,It takes V、Ni、Mo、Re、As、Cd、Uand U/Th、δU、V/(V+Ni)、V/Cr、Ni/Co as index,It is further confirmed that the slope-continental slope facies of the Niutitang formation in the study area are all located below the oxidation interface,It belongs to the environment of anaerobic reduction,To the top of this group, there is a deep-water shelf facies deposition with low oxygen and weak oxidation,Seven REDOX stages were further divided,The sedimentary environmental conditions and evolution characteristics of Niutitang formation in the study area were refined。
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