东特提斯喜马拉雅下白垩统碎屑锆石U-Pb年代学及其古地理

焦显伟; 石玉若; 杨天水; 边伟伟; 王锁; 彭文骁

doi:10.3799/dqkx.2020.308

Volume 46 Issue 8

Aug. 2021

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Article Navigation > Earth Science > 2021 > 46(8): 2850-2859

Jiao Xianwei, Shi Yuruo, Yang Tianshui, Bian Weiwei, Wang Suo, Peng Wenxiao, 2021. U-Pb Age of Detrital Zircons from Lower Cretaceous in Eastern Tethyan Himalaya and Its Paleogeography. Earth Science, 46(8): 2850-2859. doi: 10.3799/dqkx.2020.308

Citation:

Jiao Xianwei, Shi Yuruo, Yang Tianshui, Bian Weiwei, Wang Suo, Peng Wenxiao, 2021. U-Pb Age of Detrital Zircons from Lower Cretaceous in Eastern Tethyan Himalaya and Its Paleogeography. Earth Science, 46(8): 2850-2859. doi: 10.3799/dqkx.2020.308

Citation:

Jiao Xianwei, Shi Yuruo, Yang Tianshui, Bian Weiwei, Wang Suo, Peng Wenxiao, 2021. U-Pb Age of Detrital Zircons from Lower Cretaceous in Eastern Tethyan Himalaya and Its Paleogeography. Earth Science, 46(8): 2850-2859. doi: 10.3799/dqkx.2020.308

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U-Pb Age of Detrital Zircons from Lower Cretaceous in Eastern Tethyan Himalaya and Its Paleogeography

doi: 10.3799/dqkx.2020.308

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Beijing SHRIMP Center, Institute of Geology of Chinese Academy of Geological Sciences, Beijing 100083, China

Received Date: 2020-07-31
Available Online: 2021-09-14
Publish Date: 2021-08-15

Abstract

Abstract

The eastern Tethyan Himalaya is located at the combination area of eastern Gondwana during the Mesozoic, and its paleogeography plays a vital role in understanding the breakup of eastern Gondwana. A detailed chronological study of detrital zircons was carried out on the sedimentary strata in Taga area. The zircon U-Pb isotope results show that the youngest age is 126.6±2.7 Ma, suggesting that the lower limit of sampling section was the Early Cretaceous. The U-Pb age spectra of detrital zircons reveal three major age peaks at~520 Ma, ~890 Ma, and~1 200 Ma, of which the comparison with those from adjacent areas indicates similar age populations with eastern India and southwestern Australia. New results, together with the surrounding magmatic activity and the age of basalts in the lower part of sampling section, support that the studied section should be developed during the separation of the eastern Tethyan Himalayan from eastern Gondwana, and the main provenance of the sampling section might be from eastern India, southwestern Australia, and Antarctic.
- eastern Tethyan Himalaya,
- eastern Gondwana,
- detrital zircon,
- paleogeography

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References(51)

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