丁屋岭组

时代属南华纪,分布于闽南地区,为浅变质岩系。为变质石英细砂岩、粉砂岩夹千枚岩及硅质岩,底部为砾岩及含砾砂岩,中下部偶见磷质条带,厚1531米。含丰富的微古植物Trachysphaeridium sp.,Microconcentrica sp.等。与下伏楼子坝群呈假整合接触,与上覆震旦系呈整合接触。

Concept & Semantic
  10

Contributor

contributed at 2011-10-11

Classification(s)

Earth System(in Chinese)Geostratigraphic stratigraphy

Detailed Description

EN_US
Name Dingwuling Fm
ZH_CN
Name 丁屋岭组
Description 时代属南华纪,分布于闽南地区,为浅变质岩系。为变质石英细砂岩、粉砂岩夹千枚岩及硅质岩,底部为砾岩及含砾砂岩,中下部偶见磷质条带,厚1531米。含丰富的微古植物Trachysphaeridium sp.,Microconcentrica sp.等。与下伏楼子坝群呈假整合接触,与上覆震旦系呈整合接触。

How to cite

NNU_Group (2020). 丁屋岭组, Concept & Semantic, OpenGMS, https://geomodeling.njnu.edu.cn/repository/concept/a9bd7957-baa6-4e51-90a6-4b45d55d20b0
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Contributor

contributed at 2011-10-11

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