Lhasa terrane: A key piece of the supercontinent reconstruction puzzle from Rodinia to Gondwana
Here we report in detail on new U–Pb zircon dating, geochemical and Sr–Nd–Hf-O isotopic data of the late Neoproterozoic ophiolite fragments and island arc magmatic rocks from Lhasa terrane, central Tibet, China, and reveal that they generally experienced a distinctive metamorphic event (~660–650 Ma). These results, combined with previous provenance analysis, Lhasa terrane is firstly proposed to locate in the late Neoproterozoic juvenile arc system (Madagascar-Seychelles-NW India) laying either along the periphery of Rodinia or outboards of the supercontinent, recording the history of subduction and closure of the Mozambique ocean and later lateral-escape tectonics.
How to cite this dataset:
Zhang, X., Wang, Q., Dan, W., Wyman, D., 2021. Lhasa terrane: A key piece of the supercontinent reconstruction puzzle from Rodinia to Gondwana, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111791.
DOI Creation Date:
Zhang XZ, Wang Q, Dan W, Wyman D.(2021).Lhasa terrane: A key piece of the supercontinent reconstruction puzzle from Rodinia to Gondwana.Geophysical Research Letters,in review.
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Second Tibetan Plateau Scientific Expedition and Research program: STEP)
National Natural Science Foundation of China: Nos. 41872065, 41630208 and 91855215
Coverage Scope: Regional (Continents, Oceans)
User Contributed Keyword(s):
Lhasa terrane, NW India, East African Orogen, Late Neoproterozoic, Rodinia, Gondwana
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