Luliang meta-gabbro whole rock geochemistry and zircon isotope and trace elements data
Recognition of tectonic switching is of great significance for understanding the formation and evolution of ancient accretionary orogens. In this study, whole-rock geochemical and Sm-Nd isotopic, and zircon U-Pb, Lu-Hf isotopic and trace element data are reported for two generations of metamorphosed mafic rocks from the Lüliang Complex, middle Trans-North China Orogen (TNCO).
How to cite this dataset:
Liu, C. 2020. Luliang meta-gabbro whole rock geochemistry and zircon isotope and trace elements data, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111718.
DOI Creation Date:
Liu et al., Tectonic switching of the Trans-North China Orogen in the middle Paleoproterozoic: insights from mafic magmatism in the Lüliang Complex. Tectonics (accepted)
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]
- Coverage Scope: Regional (Continents, Oceans)
- Geographic Location: North China Craton
User Contributed Keyword(s):
tectonic switching, North China Craton, middle Paleoproterozoic
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