上黑龙江冒地槽褶皱带
位于黑龙江省最北部，为兴凯褶皱基底之上的燕山冒地槽褶皱带。地槽沉积主要由中侏罗统砂页岩组成，厚近10000米。我国境内主要为陆相沉积，进入俄罗斯后即以海相沉积为主，属蒙古鄂霍次克褶皱系的一部分。
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Alias
Contributor
contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Theory of polycycle
Detailed Description
| English |
|---|
| Name | Upper Heilongjiang miogeosynclinal fold belt |
| Chinese |
|---|
| Name | 上黑龙江冒地槽褶皱带 |
| Description | 位于黑龙江省最北部，为兴凯褶皱基底之上的燕山冒地槽褶皱带。地槽沉积主要由中侏罗统砂页岩组成，厚近10000米。我国境内主要为陆相沉积，进入俄罗斯后即以海相沉积为主，属蒙古鄂霍次克褶皱系的一部分。 |
How to Cite
NNU_Group (2011). 上黑龙江冒地槽褶皱带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/4b135d87-790c-4d5f-9949-11ca4d129794
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