昆仑褶皱系
为一华力西褶皱系。其范围大致与昆仑山脉一致。以阿尔金断裂为界分为两部分：东昆仑褶皱系，包括柴达木北缘优地槽褶皱带、祁曼塔格优地槽褶皱带、布尔汗布达优地槽褶皱带及柴达木盆地等构造单元。柴达木北缘为早华力西褶皱带，地槽封闭于晚泥盆世以前；祁曼塔格和布尔汗布达均为晚华力西褶皱带，地槽于早二叠世末褶皱；柴达木是一个中新生代坳陷，基底由华力西褶皱和扬子褶皱构成。西昆仑褶皱系，以一个巨型反S型褶皱山系屹立于塔里木地台之西南，向西延入塔吉克斯坦，为晚华力西地槽，早二叠世末褶皱，中新生代以来经受强烈改造，喜马拉雅运动造成今日的昆仑山系。
84
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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 | Kunlun fold system |
| Chinese |
|---|
| Name | 昆仑褶皱系 |
| Description | 为一华力西褶皱系。其范围大致与昆仑山脉一致。以阿尔金断裂为界分为两部分：东昆仑褶皱系，包括柴达木北缘优地槽褶皱带、祁曼塔格优地槽褶皱带、布尔汗布达优地槽褶皱带及柴达木盆地等构造单元。柴达木北缘为早华力西褶皱带，地槽封闭于晚泥盆世以前；祁曼塔格和布尔汗布达均为晚华力西褶皱带，地槽于早二叠世末褶皱；柴达木是一个中新生代坳陷，基底由华力西褶皱和扬子褶皱构成。西昆仑褶皱系，以一个巨型反S型褶皱山系屹立于塔里木地台之西南，向西延入塔吉克斯坦，为晚华力西地槽，早二叠世末褶皱，中新生代以来经受强烈改造，喜马拉雅运动造成今日的昆仑山系。 |
How to Cite
NNU_Group (2011). 昆仑褶皱系, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/2b758960-8449-46fa-9acc-546e00c78c60
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