地球科学进展2014,Vol.29Issue(7) :859-864.DOI:10.11867/j.issn.1001-8166.2014.07.0859

黔东北志留纪晚期小溪组沉积环境研究

A Study of the Sedimentary Environment of the Xiaoxi Formation in NE of Guizhou, China

马会珍 王雪华
地球科学进展2014,Vol.29Issue(7) :859-864.DOI:10.11867/j.issn.1001-8166.2014.07.0859

黔东北志留纪晚期小溪组沉积环境研究

A Study of the Sedimentary Environment of the Xiaoxi Formation in NE of Guizhou, China

马会珍 1王雪华1
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作者信息

  • 1. 贵州省地质调查院,贵州 贵阳550005
  • 折叠

摘要

黔东北印江合水和石阡乌谷溪的小溪组中发育良好的遗迹化石,经鉴定共计有5个属的遗迹化石:Palaeophycus isp.,Rusophycus isp.,Planolites isp.,Gordia isp.和Phycodes isp..根据遗迹化石的组合特征,该组合属于Cruziana遗迹相.结合2个剖面的沉积构造和砂岩粒度分析结果,认为小溪组的沉积环境为相对安静的平均低潮线以下的临滨带.

Abstract

The Xiaoxi Formation is well developed in two sections (Heishui,Yinjiang and Wuguxi,Shiqian),NE of Guizhou,China.This formation is composed of the sandstones,siltstones and mudstones,and preserved with the depostional structures and trace fossils.This paper focuses on the study of the sedimentary environment of the Xiaoxi Formation based on the materials from these sections.Five ichospecies are identified from two sections,including Palaeophycus isp.,Rusophycus isp.,Planolites isp.,Gordia isp.and Phycodes isp.These trace fossils belong to the Cruziana ichofacies,Based on the depositonal structures,the ichofaces and the result of particle size analysis,the sedimentary environment of the Xiaoxi Formation of Silurian in NE of Guizhou is nearshore zone with a relativealy and stable environment under the average low tide line.

关键词

小溪组/沉积环境/志留系/黔东北

Key words

Xiaoxi Formation/Sedimentary environment/Silurian/NE of Guizhou

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基金项目

中国地质调查局项目(1212011120108)

贵州省地矿局科研项目(黔地矿科200919)

出版年

2014
地球科学进展
中国科学院资源环境科学信息中心 国家自然科学基金委员会地球科学部 中国科学院资源环境科学与技术局

地球科学进展

CSTPCDCSCD北大核心
影响因子:2.045
ISSN:1001-8166
被引量11
参考文献量6
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