白兆山组
时代属震旦纪。主要分布在湖北随州、京山、安陆等地，为碳酸盐岩地层。岩石特征与扬子区有差异，主要为灰岩及白云岩和具硅质条带或结核的白云质灰岩夹硅质岩薄层，向上硅质成分增加为中厚层硅质岩。总厚419米。与下伏岔河组呈整合接触，上覆地层为含化石的寒武系余家冲组。
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Contributor
contributed at 2011-10-11
Classification(s)
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Earth System(in Chinese) Geostratigraphic stratigraphy
Detailed Description
| English |
|---|
| Name | Baizhaoshan Fm |
| Chinese |
|---|
| Name | 白兆山组 |
| Description | 时代属震旦纪。主要分布在湖北随州、京山、安陆等地，为碳酸盐岩地层。岩石特征与扬子区有差异，主要为灰岩及白云岩和具硅质条带或结核的白云质灰岩夹硅质岩薄层，向上硅质成分增加为中厚层硅质岩。总厚419米。与下伏岔河组呈整合接触，上覆地层为含化石的寒武系余家冲组。 |
How to Cite
NNU_Group (2011). 白兆山组, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/f11eaa16-d071-4be2-bffc-088e433ef9bf
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