Early middle Miocene tectonic uplift of the northwestern part of the Qinghai–Tibetan Plateau evidenced by geochemical and mineralogical records in the western Tarim Basin

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Early middle Miocene tectonic uplift of the northwestern part of the Qinghai–Tibetan Plateau evidenced by geochemical and mineralogical records in the western Tarim Basin

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作者：Chaowen Wang ; Hanlie Hong ; Hemmo A. Abels…
关键词：Tarim Basin ; Paleoclimate ; Tectonics ; Clay minerals ; Qinghai–Tibetan Plateau ; Chemical weathering
刊名：International Journal of Earth Sciences
出版年：2016
出版时间：April 2016
年：2016
卷：105
期：3
页码：1021-1037
全文大小：4,156 KB
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Zheng H, Tada R, Jia J, Lawrence C, Wang K (2010) Cenozoic sediments in the southern Tarim Basin: implications for the uplift of northern Tibet and evolution of the Taklimakan Desert. Geol Soc Lond Spec Publ 342:67–78. doi:10.1144/SP342.6 CrossRef
作者单位：Chaowen Wang (1) (2)
Hanlie Hong (1)
Hemmo A. Abels (2)
Zhaohui Li (3) (4)
Kai Cao (4)
Ke Yin (1) (4)
Bowen Song (1)
Yadong Xu (1)
Junliang Ji (1)
Kexin Zhang (1) (4)

1. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, Hubei, People’s Republic of China
2. Stratigraphy/Paleontology, Department of Earth Sciences, Utrecht University, Utrecht, 3808 TA, The Netherlands
3. Geosciences Department, University of Wisconsin - Parkside, Kenosha, WI, 53141-2000, USA
4. Faculty of Earth Sciences, China University of Geosciences, Wuhan, 430074, People’s Republic of China
刊物类别：Earth and Environmental Science
刊物主题：Earth sciences
Geology
Geophysics and Geodesy
出版者：Springer Berlin / Heidelberg
ISSN：1437-3262

文摘

The Tarim Basin in western China has been receiving continuous marine to lacustrine deposits during the Cenozoic as a foreland basin of the Qinghai–Tibetan Plateau (QTP). Clay mineralogy and geochemical proxy data from these sedimentary archives can shed light on climate and tectonic trends. Here we report on an abrupt mineralogical and weathering shift at 17 Ma ± 1 Myr in the Miocene Qimugan section in the northwestern part of the Qinghai–Tibetan Plateau. The rapid shift involves decreasing trends of chemical weathering indices, Rb/Sr and Ba/Sr ratios, and of minor and immobile elements with respect to upper crust composition as well as increasing trends of Na/Al and Na/Ti ratios, smectite, chlorite, and calcite contents. We ascribe these trends to changing source rocks due to uplift of the northern part of the QTP leading to exposures of younger intrusive bodies and older gneisses, schists, and carbonate-rich rocks. These uplifts potentially caused regional aridification reducing chemical weathering. The dating is indirect via magnetostratigraphically dated ostracod biostratigraphy and detrital zircon chronology and currently not good enough to compare the shift accurately in time with the onset of the global middle Miocene Climate Optimum (MMCO) at 16.5 Ma. Nevertheless, regional tectonics seem to have dominated over global climate as the warmer MMCO is expected to have increased weathering indices and decreased Na/Al and Na/Ti, rather than the observed reverse trends.