浓山组
时代属古新世晚期。分布于广东南雄盆地，典型剖面位于南雄大塘圩西的坪岭至古城一带。为陆相沉积，以灰绿色、紫红色砂质泥岩和泥质砂岩互层为主，含哺乳类化石Ernanodon antelios，Haltictops mirabilis，Yantanglestes datangensis等以及爬行类、介形虫、腹足类、轮藻等，厚460米。与下伏上湖组呈整合或假整合接触。
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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 | Nongshan Fm |
| Chinese |
|---|
| Name | 浓山组 |
| Description | 时代属古新世晚期。分布于广东南雄盆地，典型剖面位于南雄大塘圩西的坪岭至古城一带。为陆相沉积，以灰绿色、紫红色砂质泥岩和泥质砂岩互层为主，含哺乳类化石Ernanodon antelios，Haltictops mirabilis，Yantanglestes datangensis等以及爬行类、介形虫、腹足类、轮藻等，厚460米。与下伏上湖组呈整合或假整合接触。 |
How to Cite
NNU_Group (2011). 浓山组, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/f038fae4-6fc8-4ba6-b6c0-61acf7cb9905
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