那丹哈达优地槽褶皱带
位于我国东北部，属于锡霍特褶皱系。为一华力西褶皱基底之上的燕山优地槽褶皱带。中生代地槽型火山沉积岩沉积从晚三叠世开始，到中侏罗世晚期结束。地槽期后的沉积盖层称龙爪沟群，为海陆交互相沉积。
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Contributor
contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Theory of polycycle
Detailed Description
| English |
|---|
| Name | Nadanhada eugeosynclinal fold belt |
| Chinese |
|---|
| Name | 那丹哈达优地槽褶皱带 |
| Description | 位于我国东北部，属于锡霍特褶皱系。为一华力西褶皱基底之上的燕山优地槽褶皱带。中生代地槽型火山沉积岩沉积从晚三叠世开始，到中侏罗世晚期结束。地槽期后的沉积盖层称龙爪沟群，为海陆交互相沉积。 |
How to Cite
NNU_Group (2011). 那丹哈达优地槽褶皱带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/041209ed-4fc9-4477-8f18-3b8527606317
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