Luliang meta-gabbro whole rock geochemistry and zircon isotope and trace elements data
Abstract:
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. Accessed 2024-04-26.
DOI Creation Date:
2020-10-27
Related
Publication(s):
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)
License:
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Keyword(s):
Coverage Scope: Regional (Continents, Oceans)
Geographic Location: North China Craton
User Contributed Keyword(s):
tectonic switching, North China Craton, middle Paleoproterozoic
Data Available On:
2020-10-27