Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc

Tianyi Shen; Guocan Wang

doi:10.1007/s12583-020-1285-y

Volume 31 Issue 5

Oct 2020

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Journal of Earth Science > 2020 > 31(5): 896-904.

Tianyi Shen, Guocan Wang. Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc. Journal of Earth Science, 2020, 31(5): 896-904. doi: 10.1007/s12583-020-1285-y

Citation:

Tianyi Shen, Guocan Wang. Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc. Journal of Earth Science, 2020, 31(5): 896-904. doi: 10.1007/s12583-020-1285-y

Citation:

Tianyi Shen, Guocan Wang. Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc. Journal of Earth Science, 2020, 31(5): 896-904. doi: 10.1007/s12583-020-1285-y

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Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc

doi: 10.1007/s12583-020-1285-y

Tianyi Shen^{,
,},
Guocan Wang

School of Earth Sciences, Center for Global Tectonics, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

More Information

Corresponding author: Tianyi Shen, shenty@cug.edu.cn
Received Date: 11 Nov 2019
Accepted Date: 25 Dec 2019
Publish Date: 20 Oct 2020

Abstract

Abstract

It is still controversial how the high elevation of the Tibetan Plateau established after the Indian-Asian collision during the Cenozoic. The timing of Gangdese magmatic arc exhumation and uplift history would provide useful message for this disputation. We present six zircon fission-track (ZFT) data from modern river sand in the western Tibet,around the Mt. Kailas,to decipher the long-term exhumation histories of the Gangdese magmatic arc. The data suggests that all the Gangdese magmatic arc rocks experienced rapid cooling during the Eocene (~46-35 Ma) and Oligocene (~31-26 Ma). The movement along the north-south trending extensional fault and dextral strike-slip Karakoram fault induced the adjacent rocks exhumed at the Middle Miocene (~15-16 Ma) and Late Miocene (~10-11 Ma),respectively. According to the minimum and central AFT ages for each sample,the fastest exhumation rate is about 0.4 km/Ma,with average long-term exhumation rates on the order of~0.3 km/Ma since the Oligocene. This result supports the outward growth model for plateau forming,indicating the southern margin of the Gangdese magmatic arc attained high elevation after the Oligocene.
- detrital zircon fission-track,
- exhumation history,
- Gangdese magmatic arc,
- western Tibet

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Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc

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Detrital Zircon Fission-Track Thermochronology of the Present-Day River Drainage System in the Mt. Kailas Area, Western Tibet: Implications for Multiple Cooling Stages of the Gangdese Magmatic Arc

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