Precambrian metamorphic basement of the southern Lhasa terrane, Tibet

The Precambrian basement of the Lhasa terrane provides important information for understanding the formation and evolution of the Tibetan Plateau. However, due to the paucity of exposure, the properties of the Precambrian basement of the Lhasa terrane remain poorly known. Here we report zircon U-Pb ages, bulk-rock geochemical and zircon Hf isotopic data on the orthogneisses in the Milin area of the southeastern Lhasa terrane, southern Tibet. Inherited magmatic zircon cores of these gneisses yield protolith crystalline ages of 1556-1517 Ma, whereas the zircon rims give metamorphic ages of 1197-1192 Ma, both could be local provenance for the Mesoproterozoic detrital zircons in the Neoprotemzoic-Paleozoic strata in the Lhasa terrane. Geochemical data indicate that the protoliths of the Mesoproterozoic rocks are continental arc-like granitoids with bulk-rock epsilon(Hf)(t) values of -3.7 to +0.7 (T-DM2 = 1.99-2.34 Ga) and zircon core epsilon(Hf)(t) values of +1.8 to +8.6 (T-DM2 = 1.71-2.17 Ga), suggesting their most likely derivation from partial melting of Paleoproterozoic crustal materials. We propose that the Mesoproterozoic gneisses in the Milin area represent the Precambrian metamorphic basement of the Lhasa terrane, likely related to the growth of Columbia supercontinent. Local exposure of the Precambrian metamorphic basement may be caused by crustal rapid uplift and erosion in the late Cenozoic and their inhomogeneous distribution.

Automated summary

The study on orthogneisses in the Milin area of the southeastern Lhasa terrane provides insights into the local protolith crystalline ages and their relation to the Neoproterozoic-Paleozoic strata in the Lhasa terrane. Geochemical data suggests the Mesoproterozoic rocks may have originated from partial melting of Paleoproterozoic crustal materials, representing the Precambrian metamorphic basement of the Lhasa terrane.