库西姆契克群
又称库松木切克群。属中元古代至新元古代。分布于新疆精河县至赛里木湖以南库西姆契克山(库松木切克山)地区，为一套碳酸盐岩地层。自下而上分为：塔木契组，为单一的薄、中、厚层灰岩，厚410米；三个泉组，为含叠层石白云岩、大理岩，厚310米；四台组，为灰岩、炭质灰岩、白云质灰岩和角砾灰岩，厚800米；松树头组，为灰岩、薄层状白云岩，厚195～395米。含大量叠层石：Kussiella f.,Jacutophyton f.,Conophyton f,.等；微古植物Asperatopsophosphaera sp.,Pseudozonosphaera sp.等。上部被震旦系冰碛层不整合覆盖，未见底。松树头组时代相当青白口纪；下部三组属中元古代。
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Alias
Contributor
contributed at 2011-10-11
Classification(s)
●
Earth System(in Chinese) Geostratigraphic stratigraphy
Detailed Description
| English |
|---|
| Name | Koxemqek Gr |
| Chinese |
|---|
| Name | 库西姆契克群 |
| Description | 又称库松木切克群。属中元古代至新元古代。分布于新疆精河县至赛里木湖以南库西姆契克山(库松木切克山)地区，为一套碳酸盐岩地层。自下而上分为：塔木契组，为单一的薄、中、厚层灰岩，厚410米；三个泉组，为含叠层石白云岩、大理岩，厚310米；四台组，为灰岩、炭质灰岩、白云质灰岩和角砾灰岩，厚800米；松树头组，为灰岩、薄层状白云岩，厚195～395米。含大量叠层石：Kussiella f.,Jacutophyton f.,Conophyton f,.等；微古植物Asperatopsophosphaera sp.,Pseudozonosphaera sp.等。上部被震旦系冰碛层不整合覆盖，未见底。松树头组时代相当青白口纪；下部三组属中元古代。 |
How to Cite
NNU_Group (2011). 库西姆契克群, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/2853bbc5-fa3e-4e05-aaa4-4d254bc43062
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