特提斯喜马拉雅-印度地体初始裂解:来自藏南地区晚白垩世OIB型玄武岩的证据

黄勇; 梁维; 张林奎; 李光明; 黄春梅; 夏祥标; 董随亮; 吴建阳

doi:10.3799/dqkx.2017.573

Volume 43 Issue 8

Aug. 2018

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Article Navigation > Earth Science > 2018 > 43(8): 2651-2663

Huang Yong, Liang Wei, Zhang Linkui, Li Guangming, Huang Chunmei, Xiao Xiangbiao, Dong Suiliang, Wu Jianyang, 2018. The Initial Break-Up between Tethyan-Himalaya and Indian Terrane: Evidences from Late Cretaceous OIB-Type Basalt in Southern Tibet. Earth Science, 43(8): 2651-2663. doi: 10.3799/dqkx.2017.573

Citation:

Huang Yong, Liang Wei, Zhang Linkui, Li Guangming, Huang Chunmei, Xiao Xiangbiao, Dong Suiliang, Wu Jianyang, 2018. The Initial Break-Up between Tethyan-Himalaya and Indian Terrane: Evidences from Late Cretaceous OIB-Type Basalt in Southern Tibet. Earth Science, 43(8): 2651-2663. doi: 10.3799/dqkx.2017.573

Citation:

Huang Yong, Liang Wei, Zhang Linkui, Li Guangming, Huang Chunmei, Xiao Xiangbiao, Dong Suiliang, Wu Jianyang, 2018. The Initial Break-Up between Tethyan-Himalaya and Indian Terrane: Evidences from Late Cretaceous OIB-Type Basalt in Southern Tibet. Earth Science, 43(8): 2651-2663. doi: 10.3799/dqkx.2017.573

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The Initial Break-Up between Tethyan-Himalaya and Indian Terrane: Evidences from Late Cretaceous OIB-Type Basalt in Southern Tibet

doi: 10.3799/dqkx.2017.573

1.
Chengdu Center of China Geological Survey, Chengdu 610081, China
2.
School of Earth Science and Resource, China University of Geosciences, Beijing 100083, China

Received Date: 2017-12-16
Publish Date: 2018-08-15

Abstract

Abstract

The initial break-up time between Tethyan-Himalaya and Indian terrane has been controversial for a long time.In this study, we report newly discovered pillow basalts which provide new insights to the solution of the problem.The pillow basalts trending northwestward unconformable overlap on the Middle Jurassic Zhela Formation.The zircon SHRIMP U-Pb isotopic dating shows the formation age of 92.1±1.2 Ma, representing the Late Cretaceous volcanic activity of the Tethys Himalaya.The major and trace elements analyses show the basalt is alkaline basalt with (La/Yb)_N=5.7~7.1 and without Nb-Ta, Eu, Zr-Hf negative anomalies, and it has high Fe, P, Ti contents, low (La/Nb)_PM and (Th/Ta)_PM ratios.Zircon ε_Hf(t) values range from 9.02 to 12.97, with an average of 10.50 and t_DM1 is 241-399 Ma.Geochemical and isotopic data show that the Kada basalt is OIB-type basalt without any contamination from the crust and the magma originates from partial melting of garnet-spinel bearing lherzolite.Kada basalt is present within Tethyan Himalaya passive continental margin.Mafic volcanics spreading within passive continental margins is usually related with the processes of continental break-up and formation of a new ocean basin.Combined with the latest research result of paleomagnetic and evolution of Neo-Tethys oceanic basin, we suggest that the Kada basalt is related to the initial break-up between Tethyan-Himalaya and Indian terrane.The Kada basalt provides new clues for the study of tectonic evolution of the Tethyan Himalaya.
- Late Cretaceous,
- OIB-type basalt,
- initial break-up,
- Tethyan-Himalaya,
- U-Pb dating,
- geochemistry,
- geochronology

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References(62)

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The Initial Break-Up between Tethyan-Himalaya and Indian Terrane: Evidences from Late Cretaceous OIB-Type Basalt in Southern Tibet

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