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).

Other Description: 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)