首页> 外文会议>International Symposium on the Cambrian System and Field Conference of the Cambrian Stage Subdivision Working Group; 200508; Nanjing(CN) >EDIACARAN-CAMBRIAN BOUNDARY SECTION AT ZHUJIAQING, NEAR DAHAI, HUIZE COUNTY, YUNNAN, CHINA: POTENTIAL STRATOTYPE SECTION FOR SUBDIVISION OF THE FIRST SERIES OF THE CAMBRIAN
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EDIACARAN-CAMBRIAN BOUNDARY SECTION AT ZHUJIAQING, NEAR DAHAI, HUIZE COUNTY, YUNNAN, CHINA: POTENTIAL STRATOTYPE SECTION FOR SUBDIVISION OF THE FIRST SERIES OF THE CAMBRIAN

机译:云南省会泽县大海市附近的朱家Q的EDIACARAN-CAMBRIAN边界断面:可能的地层原型剖面被细分为第一系列的寒武纪

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摘要

The Zhujiaqing section is the type section of the Zhujiaqing Formation. Which is located near Dahai, Huize County, Yunnan, China. The contact with the underlying Tongying Formation is marked by the disappearance of the light-gray, thick-bedded dolostone of the Tongying Formation and the first occurrence of dark-gray, thin- to medium-bedded, siliceous dolostone and silicastone of the Daibu Member. The upper boundary is marked by a glauconite-bearing sandstone at the base of the overlying Shiyantou Formation. The glauconite-bearing sandstone bed is overlain by a volcanic ash layer (bentonite).
机译:朱家卿断面是朱家卿组的典型断面。位于中国云南会泽县大海附近。与下面的同营组的接触以同营组的浅灰色,厚层白云岩消失和代步组首次出现的深灰色,薄至中层,硅质白云岩和二氧化硅岩为标志。 。上界由上覆的石岩头组底部含钙云母的砂岩标记。含青石岩的砂岩床被火山灰层(膨润土)覆盖。

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