financially supported by the Basic Foundation of Tianjin University of Commerce;the Fund from the Key Laboratory of Continental Dynamics of Ministry of Natural Resources(J2306)。
Deciphering high-pressure granulite-facies metamorphism and anatexis within a collisional orogeny can provide crucial constraints on geodynamic evolution and melt activity during subduction and exhumation.Combining pe...
supported by National Natural Science Foundation of China(Nos.42072228,42102060,41902036,41572182);China Postdoctoral Science Foundation(No.2021M692983);the Chinese Ministry of Education(No.BP0719022);the Most Special Fund(Nos.MSFGPMR02-3,MSFGPMR30);Open funds from the State Key Laboratory of Geological Processes and Mineral Resources;China University of Geosciences(Nos.GPMR201703,GPMR201704 and GPMR201903);the Fundamental Research Funds for National University(No.CUG-G1323511572)。
‘Single shot'laser-ablation split-stream(SS-LASS)technique analyzing unpolished zircon grains makes their thin rims tenable for determination,which thus offers great potential in deciphering the timing of multiple an...
Dehydration melting of metasupracrustal rocks at mid-to deep-crustal levels can generate water undersaturated granitic melt.In this study,we evaluate the potential of~1.89–1.88 Ga metasupracrustal rocks of the Precam...
The CAGS Research Fund(YYWF201715,YK1608);the project of China Geological Survey(DD20190437)financially support this study and contribution.
Two Neoarchean alkaline feldspar-rich granites sourced from partially melted granulite-facies granodioritic orthogneiss have been here recognised in the eastern part of the North China Block(NCB).These poorly foliated...
funded by the National Key R&D Program of China(grant numbers 2019YFC0605202 and 2019YFC0605203);Geological Survey Project grants from the China Geological Survey(grant numbers 12120113102100,DD20160056);Research Program of Department of Land and Resources of Hunan Province(grant number 2018-02);the Chinese National Non-Profit Institute Research Grant of CAGS-IMR(grant number IMRKK1927);the National Natural Science Foundation of China(41872096);the Chinese National Non-profit Institute Research Grant of CAGS(JYYWF201814)。
The Berere HTHP Complex belt in Maevatanana area of north–central Madagascar formed in the^2.5 Ga orogeny and underwent high temperature(up to 1050℃)and high pressure(up to 11.5 kbar)granulite facies metamorphism.Th...
funded by a National Sciences and Engineering Research Council of Canada Discovery grant to CY;supported by a Vanier Canada Graduate Scholarship。
Tonalite-trondhjemite-granodiorite(TTG) suites constitute a large proportion of the Archean geological record;however,the geodynamic processes that generated them,and Archean continental crust in general,remain a subj...
financially supported by the National Natural Science Foundation of China (41872194, 41872203)
The Neoarchean charnockites of North margain of North China Craton(NCC) has become a hot topic into understanding the Early Precambrian basement. Although there is a broad consensus that charnockite is usually related...
The Higher Himalayan Crystallines(HHC), in western Garhwal, Uttarakhand are located in a regionalscale intracontinental ductile shear zone(15-20 km wide) bounded by the Main Central Thrust at the base, and the South T...
supported by the National Natural Science Foundation of China (Grant Nos. 41630207, 41572180);the China Geological Survey Project (Grant No. 12120115027001)
In the northern West Qinling orogen(WQO), granulite-facies metamorphic rocks are recognized within the Qinling Complex. These rocks are composed of amphibole-bearing two-pyroxene granulite and garnet-sillimanite gneis...
supported by the National Natural Science Foundation of China (Grant No. 41430207)
It is generally believed that trondhjemitic rock, an important component of TTG rocks, is the anatectic product of mafic rocks. However, in many TTG gneiss terranes, for instance, the granulite facies terrane in Easte...