曲靖组
时代属中泥盆世东岗岭期。广泛分布于滇东、滇东北、滇东南地区。为一套巨厚的碳酸盐岩地层，主要由灰色中—厚层灰岩、泥灰岩、白云岩、白云质灰岩及生物灰岩组成。层位介于一打得组黑色页岩与海口组砂岩之间，与下伏海口组呈整合接触。厚1312米。富含底栖腕足类Stringocephalus，珊瑚Temnophyllum，层孔虫、介形虫等化石。
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Alias
Contributor
contributed at 2011-10-11
Classification(s)
●
Earth System(in Chinese) Geostratigraphic stratigraphy
Detailed Description
| English |
|---|
| Name | Qujing Fm |
| Chinese |
|---|
| Name | 曲靖组 |
| Description | 时代属中泥盆世东岗岭期。广泛分布于滇东、滇东北、滇东南地区。为一套巨厚的碳酸盐岩地层，主要由灰色中—厚层灰岩、泥灰岩、白云岩、白云质灰岩及生物灰岩组成。层位介于一打得组黑色页岩与海口组砂岩之间，与下伏海口组呈整合接触。厚1312米。富含底栖腕足类Stringocephalus，珊瑚Temnophyllum，层孔虫、介形虫等化石。 |
How to Cite
NNU_Group (2011). 曲靖组, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/1c2d7064-0ef0-4ba2-a502-4f9d628c55e8
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