| 贵州黔东地区中-下寒武统凯里组发育特征 |
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| 引用本文： | 彭进. 贵州黔东地区中-下寒武统凯里组发育特征[J]. 贵州工业大学学报(自然科学版), 2002, 31(1): 7-13 |
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| 作者姓名： | 彭进 |
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| 作者单位： | 贵州工业大学教务处,贵州,贵阳,550003 |
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| 基金项目： | 国家自然科学基金 (4 9772 0 85 )，攀登专项 (95 -专 -0 1)，贵州省省长基金资助项目 . |
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| 摘 要： | 贵州黔东地区中－下寒武统凯里组主要由粉砂质泥岩，页岩及灰岩组成，富产三叶虫，其中台江八郎乌溜－曾家岩的凯时组含著名的中寒武世凯里生物群、早寒武世台江生物群，2001年成为国际中－下寒武统层型界线候选部，对其深入研究具有重大科学和实用意义。就我省黔东地区凯里组的岩石地层，生物地层，年代地层，沉积环境等进行研究及总结，亦确认黔东凯里组是一个十分重要的地层单位。
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| 关 键 词： | 凯里组 中－下寒武统 界线 凯里生物群 贵州 地层 黔东地区 发育特征 |
| 文章编号： | 1009-0193(2002)01-0007-07 |
The Lithostratigraphic,Biostratigraphic and Chronostratigraphic Characteristics of Low-Middle Cambrian Kaili Formation in Eastern Guizhou,China |
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| PENG Jin. The Lithostratigraphic,Biostratigraphic and Chronostratigraphic Characteristics of Low-Middle Cambrian Kaili Formation in Eastern Guizhou,China[J]. Journal of Guizhou University of Technology(Natural Science Edition), 2002, 31(1): 7-13 |
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| Authors: | PENG Jin |
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| Abstract: | The Kaili formation in Eastern Guizhou,China is mainly made up of silty mudstone and shales abundant in trilobites.Kaili formation,located at Wuliu Zengjiayan section of Balang,Taijiang county,as a candidate section of GSSP for Lower Middle Cambrian boundary,is famous for its Middle Cambrian Kaili biota and Lower Cambrian Taijiang biota.This paper conducts a study on the lithostratigraphic,biostratigraphic and chronstratigraphic characteristics and sedimentary environments of Kaili formation,and draws a conclusion that Kaili formation is an important stratigraphic unit because of its scientific and practical significance. |
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| Keywords: | Kaili formation Lower Middle Cambrian boundary Kaili biota Guizhou |
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