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- Publisher
- Wiley
- Copyright
- Copyright © 1993 Wiley Subscription Services, Inc., A Wiley Company
- ISSN
- 1000-9515
- eISSN
- 1755-6724
- DOI
- 10.1111/j.1755-6724.1993.mp6001001.x
- Publisher site
- See Article on Publisher Site
Abstract
Abstract Studies of the deformation styles, formation types and isotopic age data indicate that the Altaides has successively experienced 5 stages of orogeny: (1) the Kanas orogeny forming the angular unconformity between the Baihaba Formation (O3) and the Habahe Group (Z‐O2); (2) the Daqiao orogeny (S3‐D1‐2) giving rise to the early Hercynian quasi‐aulacogen extensional continental crust of the area; (3) the Altay orogeny (middle‐ late Hercynian) leading to the oblique intracontinental collision and the formation of large shear arc‐shaped thrust system and representing a strong orogeny stage; (4) the pan‐Altay orogeny (latest Hercynian‐Indosinian) resulting in the uplifting and erosion of the mountains as a whole; (5) the Himalayan movement causing the rejuvenation of fault systems and block uplift of the Altaides since the Cenozoic.
Journal
Acta Geologica Sinica (English Edition) – Wiley
Published: Jan 1, 1993
Keywords: ;