首页> 外文会议>International Symposium on the Cambrian System >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:珠家 - 朱家庆的埃德拉康 - 寒武纪边界段,云南云南霍泽县附近:中国寒武纪的第一个系列分区的潜在划线部分

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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:朱家庆部分是朱家庆的形成。位于中国云南湖化县的大海县附近。与潜在的榫卵形成的接触是由榫胶形成的浅灰色,厚床Dolostone的消失和暗灰色,薄灰色至中等床,硅质天鹅酮和Daibu成员的硅硅烷的消失。上边界标有覆盖的石岩沟地层底座的含胶石岩砂岩。携带葡糖岩砂岩床由火山灰层(膨润土)俯仰。

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