supported by the National Basic Research Program of China(2009CB825002);the National Natural Science Foundation of China(40773013 and 91014007)
Systematical studies of post-collisional igneous rocks in the Dabie orogen suggest that the thickened mafic lower crust of the orogen was partially melted to form low-Mg#adakitic rocks at 143–131 Ma.Delamination and ...
supported by the National Natural Science Foundation of China(Grant Nos.90814008,40634023 and 40973043);the National Basic Research Program of China (Grant No.2009CB825002)
We report zircon U-Pb geochronology,geochemistry and Sr-Nd-Pb isotope data from mafic granulites and garnet amphibolites of the Wuhe Complex in the southeastern margin of the North China Craton (NCC).In combination wi...
supposed bv the National Natural Science Foundation of China(Grant Nos.90814008,40634023 and 40973043);the National Basic Research Program of China(Grant No. 2009CB825002);Critical reviews and many useful suggestions by Prof.M.Santosh,Prof.Guochun Zhao(University of Hong Kong);an anonymous reviewer have greatly improved the final version of the manuscript
The crustal growth of the North China Craton (NCC) during the Neoarchean time (2.5--2.8 Ga) is a hotly controversial topic, with some proposing that the main crustal growth occurred in the late Neoarch- ean (2.5-...