partially financially supported by the National Natural Science Foundation of China(No.42002068);the MOST Special Fund from the State Key Laboratory of GPMR,China University of Geosciences(Wuhan);the 111 Project(No.BP0719022)。
Ultrahigh-pressure metamorphism has recently been reported from various crustal rocks in the Seve Nappe Complex(SNC)in which microdiamonds were found.However,in gneiss from the Lower Seve Nappe(LSN),neither any direct...
supported by the National Natural Science Foundation of China(No.41602234);the Fundamental Research Funds for the Central Universities,China University of Geosciences,Wuhan,China(Nos.CUGL180406,CUGCJ1707);Open Fund(No.GRMR201901)from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan
Electron probe microanalysis(EPMA) dating of monazite has been developed over decades. However, limited by the detectability and analytical sensitivity of dating-related elements(Th, Pb, U and Y), the EPMA dating has ...
supported by Russian Foundation for Basic Research(project 10-05-00040 to OGS);Russian President Grants for Young Scientists(MD-222.2012.5 to OGS);grant from the National Science Foundation of South Africa(GUN:20531 92 to DDvR);University of Johannesburg as a part of the Russian South African scientific collaboration
Reaction textures and fluid inclusions in the -2.0 Ga pyroxene-bearing dehydration zones within the Sand River biotite-hornblende orthogneisses (Central Zone of the Limpopo Complex) suggest that the formation of the...
supported jointly by the National Natural Science Foundation of China (Grant Nos. 41030423,41072068 and 40872071);National Basic Research Program of China (Grant No. 2006CB403502);MOST Special Fund from the State Key Laboratory of Continental Dynamics, Northwest University (Grant No. BJ091349);National Found for Fostering Talents of Basic Sciences (Grant No. J0830519);Graduate Innovation and Creativity Funds of Northwest University,China (Grant No. 10YZZ24)
The Dehe granitic pluton intruded the Xiahe Group which is in the core complex of the North Qinling Orogenic Belt(NQOB).It shows gneissic bedding and possesses typical S-type granite minerals such as muscovite and gar...
This work was sponsored by the State Key Basic Research and Development Program of China (Grant No. G1998040800); GeoForschungsZentrum in Germany for International Cooperation and the Foundation of the Opened Laboratory of Constitution; Interaction and
Here we present the results of dehydration melting, melt morphology and fluid migration based on the dehydration melting experiments on natural bio-tite-plagioclase gneiss performed at the pressure of 1.0-1.4 GPa, and...
High P_T experiment with natural massive rock sample of garnet biotite plagioclase gneiss indicates that the metamorphic reaction involving melt (reaction between relic mineral phase and melt) is the most important re...