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The Archean Kongling Complex in the northern Yangtze Craton is an ideal target to investigate the Precambrian accretion and evolution of continental crust in South China. This study aims to unravel the crustal evolution and tectonic setting of the Yangtze Craton during the Paleoproterozoic time, using integrated studies of petrography, zircon U–Pb and Hf isotopes and whole-rock geochemistry of Paleoproterozoic...
It is generally recognized that the North China Craton (NCC) resulted from the amalgamation of several micro-blocks during the Paleoproterozoic period. However, how the lower crust beneath the craton evolved during the amalgamation of these blocks is less well-known. Four garnet-bearing felsic granulite xenoliths entrained by the Mesozoic Xinyang volcanic rocks at the southwestern part of the Eastern...
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