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微量元素在华南武陵统沉积环境和物源分析中的应用

裴羽 何幼斌 曾艳涛 文沾 王宁

海相油气地质Issue(2):29-36,8.
海相油气地质Issue(2):29-36,8.DOI:10.3969/j.issn.1672-9854.2015.02.005

微量元素在华南武陵统沉积环境和物源分析中的应用

Application of Trace Elements in Analysis of Sedimentary Environments and Provenance of Wulingian Series, South China

裴羽 1何幼斌 1曾艳涛 1文沾 1王宁1

作者信息

  • 1. 长江大学地球科学学院
  • 折叠

摘要

Abstract

Cambrian Wulingian Series is distributed widely in South China, which shows southeastward deepening marine sedimentary environments that are carbonate platform, carbonate platform edge, upper slope, lower slope and basin in sequence in NE-SW zonal distribution. Rock samples are selected from western Hubei, central Hunan, and southern Hunan-southern Jiangxi areas. The geochemical characteristics of trace elements and REE in samples indicates that the whole South China was in an oxygen-poor to anaerobic marine environ ment but an oxidic environment locally in western Hubei during Wulingian Epoch. Water was perhaps shallower in depth in southern Hunan-southern Jiangxi area than that in the central Hunan area, which means possible existence of an ancient land in the southeast of South China. It is implied that the sediment provenance was derived sta bly from the upper crust in the northwest and the provenance area probably is under the tectonic setting of continental island arc or the active continental margin.

关键词

寒武纪/武陵世/微量元素/沉积环境/物源/华南

Key words

Cambrian/Wulingian Series/Trace element/Sedimentary environment/Provenance/South China

分类

能源科技

引用本文复制引用

裴羽,何幼斌,曾艳涛,文沾,王宁..微量元素在华南武陵统沉积环境和物源分析中的应用[J].海相油气地质,2015,(2):29-36,8.

基金项目

本文受中国地质科学院项目"主要地质单元区域地质调查与片区总结"(编号1212011120115)资助 (编号1212011120115)

海相油气地质

OA北大核心CSCDCSTPCD

1672-9854

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