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- Publisher
- Wiley
- Copyright
- 2006 Geological Society of China
- ISSN
- 1000-9515
- eISSN
- 1755-6724
- DOI
- 10.1111/j.1755-6724.2006.tb00263.x
- Publisher site
- See Article on Publisher Site
Abstract
Abstracts of Acta Geologica Sinica (Chinese Edition) Vol. 80, No. 5,2006 Space-Time Coordinate of the Evolution and Reformation and Mineralization Response in the Ordos Basin LIU Chiyang, ZHAO Hongge, GUI Xiaojun, YUE Leping, ZHAO Junfeng and WANG Jianqiang (State Key Laboratory of Continental Dynamics (Northwest University), Institute of Oil and Gas of Northwest University, Xi'an, Shannxi 710069) The Ordos Basin developed during the middle-late Triassic and early Cretaceous and has been reformed since the late Cretaceous. It mainly possesses the intra-craton characters and is a residual basin with multi-stage and different reformation. The Ordos Basin also belongs to a multi-superimposed basin that overlapped early and late Paleozoic basins. Therefore, multi-energy mineral deposits are abundant and petroleum, coal and uranium formed in this basin. According to the main geological structure features and geological events in the Ordos Basin and peripheral areas, together with comprehensive research of fission track ages in various district of the basin, the paper concludes that there exist at least four evident stages of structural fluctuation during the basin development and also four stages of evolution and sedimentation in the basin. The Middle-late Triassic and early-middle Jurassic Fuxian and Yan'an stages are the two most prosperous
Journal
Acta Geologica Sinica (English Edition) – Wiley
Published: Jun 1, 2006