Climatic and tectonic evolution in the North Qaidam since the Cenozoic: Evidence from sedimentology and mineralogy
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Title
Climatic and tectonic evolution in the North Qaidam since the Cenozoic: Evidence from sedimentology and mineralogy
Authors
Keywords
clay mineral, illite crystallinity, paleoclimate, Qaidam Basin, Tibetan Plateau
Journal
Journal of Earth Science
Volume 24, Issue 3, Pages 314-327
Publisher
Springer Nature
Online
2013-06-03
DOI
10.1007/s12583-013-0332-3
References
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Related references
Note: Only part of the references are listed.- The early-Eocene climate optimum (EECO) event in the Qaidam basin, northwest China: clay evidence
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- Climatic and tectonic uplift evolution since ~7 Ma in Gyirong basin, southwestern Tibet plateau: clay mineral evidence
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- (2008) A. Yin et al. GEOLOGICAL SOCIETY OF AMERICA BULLETIN
- Tibetan uplift prior to the Eocene-Oligocene climate transition: Evidence from pollen analysis of the Xining Basin
- (2008) G. Dupont-Nivet et al. GEOLOGY
- Palynological evidence for the Mid-Miocene Climatic Optimum recorded in Cenozoic sediments of the Tian Shan Range, northwestern China
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- Cenozoic sedimentary records and geochronological constraints of differential uplift of the Qinghai-Tibet Plateau
- (2008) KeXin Zhang et al. Science in China. Series D, Earth sciences / Chinese Academy of Sciences
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