渔山尖组
时代属中侏罗世。分布于浙西浦江、兰溪一带。命名地点在浙江兰溪渔山尖。为内陆河湖相沉积，岩性为暗紫色，黄绿色细砂岩、粉砂岩、泥岩，顶部为块状砾岩，含植物化石Coniopteris hymenophylloides，Cladophlebis denticulata，Baiera gracilis，Pagiophyllum sp.及双壳类Tutuella sp.，Pseudocardinia sp.，厚3020米。与下伏下侏罗统马涧组呈整合接触。
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Alias
Contributor
contributed at 2011-10-11
Classification(s)
●
Earth System(in Chinese) Geostratigraphic stratigraphy
Detailed Description
| English |
|---|
| Name | Yushanjian Fm |
| Chinese |
|---|
| Name | 渔山尖组 |
| Description | 时代属中侏罗世。分布于浙西浦江、兰溪一带。命名地点在浙江兰溪渔山尖。为内陆河湖相沉积，岩性为暗紫色，黄绿色细砂岩、粉砂岩、泥岩，顶部为块状砾岩，含植物化石Coniopteris hymenophylloides，Cladophlebis denticulata，Baiera gracilis，Pagiophyllum sp.及双壳类Tutuella sp.，Pseudocardinia sp.，厚3020米。与下伏下侏罗统马涧组呈整合接触。 |
How to Cite
NNU_Group (2011). 渔山尖组, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/48880d16-5011-48c3-b36b-2c56dbdee74e
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