| 四川峨眉高桥震旦系—寒武系界线 |
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| 引用本文： | 殷继成,丁莲芳,何廷贵,林昌宝.四川峨眉高桥震旦系—寒武系界线[J].地球学报,1980,2(1):59-74. |
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| 作者姓名： | 殷继成 丁莲芳 何廷贵 林昌宝 |
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| 作者单位： | 成都地质学院;成都地质学院;成都地质学院;成都地质学院 |
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| 摘 要： | <正> 一、前言 四川峨眉高桥震旦系—寒武系界线剖面位于峨眉山东麓。其大地构造位置居川滇南北向构造带东侧,扬子台背斜西部边缘地带。这里震旦纪和寒武纪地层广泛发育,构造简单,沉积连续,化石丰富,交通方便,是研究震且系与寒武系界线比较理想的地区之一。
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ON THE SINIAN-CAMBRIAN BOUNDARY IN EMEICOUNTY,SICHUAN |
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| YIN Ji-cheng,DING Lian-fang,HE Ting-gui and LIN Chang-bao.ON THE SINIAN-CAMBRIAN BOUNDARY IN EMEICOUNTY,SICHUAN[J].Acta Geoscientia Sinica,1980,2(1):59-74. |
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| Authors: | YIN Ji-cheng DING Lian-fang HE Ting-gui and LIN Chang-bao |
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| Institution: | Chengdu Geologic College;Chengdu Geologic College;Chengdu Geologic College;Chengdu Geologic College |
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| Abstract: | The boundary section between Sinian and Cambrian at Gaoqiao in Emeicounty of Sichuan Province is one of the important section in studying thementioned boundary in China because of its simplicity of structure, the conti-nuity of stratigraphic sequence and the abundance of fossils. This paper introduces systematically the research history of the Sinianand Cambrian, the subdivision of strata and organisms concerned in the areanear Mt. Emei. It also describes the sedimentary environments, the evolution of organisms from the late Sinian to the beginning of early Cambrian. The authors consider the first appearance of enormous amount of various kinds of shell fossils as the principal basis for the division of Sinian and Cambrain. The small-sized shelly fossils-Anarbarities-Circotheca, which represent the fossil assemblage in the lower part of the Maidiping Formation, attest to the presence of the lowest part of Cambrain. These can be correslated with contemporaneous strata and boundaries in different districts of China as well as in different parts of the world. |
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