The evolution of Lhasa terrane in the Late Paleozoic: constraints from the middle Permian magmatism in central Lhasa, Tibet
Abstract:
This is a dataset includ whole-rock major (wt. %) and trace (ppm) element, zircon U–Pb isotope, zircon trace element (ppm), zircon Lu–Hf isotope and whole-rock Sr–Nd isotope of the Tangjia high-Mg quartz diorite and Sumdo trondhjemite in central Lhasa, Tibet.
How to cite this dataset:
Wang, B., 2021. The evolution of Lhasa terrane in the Late Paleozoic: constraints from the middle Permian magmatism in central Lhasa, Tibet, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.26022/IEDA/112194. Accessed 2024-07-26.
DOI Creation Date:
2021-12-10
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Tibet
User Contributed Keyword(s):
subduction, fluids and/or melts of oceanic crust/sediment, mantle melting
Data Available On:
2021-12-11