雷口坡组
时代属中三叠世青岩期。分布于四川南部及贵州北部。命名地点在四川威远新场附近的雷口坡。为湖相沉积，以浅灰色至深灰色白云岩及灰岩为主，夹页岩和石膏层，厚约220米。下部白云质灰岩夹少许页岩，含双壳类Eumorphotis illyrica等；上部泥质白云岩、薄层灰岩及泥灰岩，含菊石Progonoceratites pulcher。与下伏嘉陵江组呈整合接触。
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Contributor
contributed at 2011-10-11
Classification(s)
●
Earth System(in Chinese) Geostratigraphic stratigraphy
Detailed Description
| English |
|---|
| Name | Leikoupo Fm |
| Chinese |
|---|
| Name | 雷口坡组 |
| Description | 时代属中三叠世青岩期。分布于四川南部及贵州北部。命名地点在四川威远新场附近的雷口坡。为湖相沉积，以浅灰色至深灰色白云岩及灰岩为主，夹页岩和石膏层，厚约220米。下部白云质灰岩夹少许页岩，含双壳类Eumorphotis illyrica等；上部泥质白云岩、薄层灰岩及泥灰岩，含菊石Progonoceratites pulcher。与下伏嘉陵江组呈整合接触。 |
How to Cite
NNU_Group (2011). 雷口坡组, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/3994e2fc-8003-4ac2-891c-0d1c3009c87c
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