Geochemistry of Punctuated orogeny during the assembly of Asia: Tectonostratigraphic evolution of the North China craton and the Qilian Shan from Paleoproterozoic to Early Paleozoic
Abstract:
Whole rock geochemistry from the northern Tibetan Plateau, eastern Qilian Shan and Longshoushan. Samples range in age from Paleozoic to Proterozoic. Granitoid and volcanic rock samples were analyzed for major and trace elements at the Chinese Academy of Geologic Sciences in Beijing, China. Major elements were analyzed using an X-ray fluorescence spectrometer. Trace elements were measured on an inductively coupled plasma-mass spectrometry (ICP-MS).
How to cite this dataset:
Wu, C., Zuza, A. V., Yin, A., Chen, X., Haproff, P. J., Li, J., Li, B., Ding, L., 2020. Geochemistry of Punctuated orogeny during the assembly of Asia: Tectonostratigraphic evolution of the North China craton and the Qilian Shan from Paleoproterozoic to Early Paleozoic, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA).
https://doi.org/10.26022/IEDA/111780. Accessed 2024-04-26.
DOI Creation Date:
2020-12-16
Related
Publication(s):
Wu, C., Zuza, A.V., Yin, A., Chen, X.H., Haproff, P.J., Li, J., Li, B., Ding, L., (2020). Punctuated orogeny during the assembly of Asia: Tectonostratigraphic evolution of the North China craton and the Qilian Shan from Paleoproterozoic to Early Paleozoic. Tectonics (in revision)
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Tibetan Plateau, western China
User Contributed Keyword(s):
Longhsoushan, Qilian Shan, Qilian orogen, North China craton, Qilian arc, Tibetan Plateau
Data Available On:
2020-12-17