| Citation: | Yan Cao, Zhiqiang Kang, Feng Yang, Tong Zhou, Dongmei Liu, Rui Wang. Geochronology, Geochemistry and Geological Significance of Volcanic Rocks of the Bangba District, Western Segment of the Central Lhasa Subterrane. Journal of Earth Science, 2022, 33(3): 681-695. doi: 10.1007/s12583-022-1634-0
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The Lhasa terrane records voluminous magmatism related to the subduction of the Neo-Tethyan oceanic lithosphere, the study of which constrains the tectonomagmatic evolution of the region. We report zircon U-Pb ages, whole-rock compositions and Sr-Nd isotopic data from volcanic rocks in the Bangba district within the central Lhasa subterrane to constrain their magmatic source and petrogenesis. Zircon U-Pb dating of two volcanic rock samples yields End Cretaceous ages of 70.0 ± 0.8 and 74.3 ± 1.2 Ma. The rocks have high SiO2 (65.41 wt.%–68.45 wt.%), Al2O3 (16.16 wt.%–16.59 wt.%) and K2O (5.00 wt.%–6.73 wt.%) contents, and low TFe2O3 (2.33 wt.%–2.79 wt.%), MgO (0.64 wt.%–1.44 wt.%) and TiO2 (0.61 wt.%–0.65 wt.%) contents, with aluminium saturation indices (A/CNK) of 0.99–1.06. The major- and trace-element compositions of the rocks show they are metaluminous to slightly peraluminous high-K calc-alkaline trachydacite. The relatively high SiO2 and Sr-Nd isotopic compositions ((87Sr/86Sr)i = 0.722 654, 0.722 038 and 0.725 787 and
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