飞仙关组
曾称飞仙关页岩。时代属早三叠世殷坑期(印度期)。分布于川西、川西北、滇东及黔西一带。命名地点在四川广元以北15千米的飞仙关。为滨海相或浅海相泥砂质沉积，以暗紫色、绿色页岩及砂岩为主，厚230～500米。上部以含双壳类Eumorphotis为最多，称Eumorphotis multiformis带；下部含Claraia为最多，称Claraia wangi带。与下伏上二叠统大隆组呈整合接触。
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Alias
Contributor
contributed at 2011-10-11
Classification(s)
●
Earth System(in Chinese) Geostratigraphic stratigraphy
Detailed Description
| English |
|---|
| Name | Feixianguan (Feisienkuan) Fm |
| Chinese |
|---|
| Name | 飞仙关组 |
| Description | 曾称飞仙关页岩。时代属早三叠世殷坑期(印度期)。分布于川西、川西北、滇东及黔西一带。命名地点在四川广元以北15千米的飞仙关。为滨海相或浅海相泥砂质沉积，以暗紫色、绿色页岩及砂岩为主，厚230～500米。上部以含双壳类Eumorphotis为最多，称Eumorphotis multiformis带；下部含Claraia为最多，称Claraia wangi带。与下伏上二叠统大隆组呈整合接触。 |
How to Cite
NNU_Group (2011). 飞仙关组, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/dd376079-3082-40d2-8879-07155224fddf
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