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 the Natural Science Foundation of Shandong Provence(Grant No.ZR2023MD058);National Natural Science Foundation of China(Grant Nos.42072219,41802201)。
The Yishui complex,located in the western Shandong area of the North China Craton,is representative of the Archean crystalline basement of the North China Craton to explore the early tectonic-thermal evolution history...
supported by the Natural Science Foundation of China(Nos.41673030,41590624);the Strategy Guide Project B of the Chinese Academy of Sciences(No.XDB18020303);the Youth Innovation Promotion Association of CAS(No.2013283);the Fundamental Research Programs for the Central Universities。
Zircon is a key accessary mineral for metamorphic geochronology and geochemical tracing,but it has been a challenge to interpret its complex chemical zoning and age record acquired during multiple episodes of anatecti...
supported by the National Natural Science Foundation of China[42025204,41890831,41803029,41973025 and 92155306];Guangdong Province Introduced Innovative R&D Team of Geological Processes and Natural Disasters around the South China Sea[2016ZT06N331];HKU Seed Fund for Basic Research[201811159089].
Ultrahigh-temperature(UHT)metamorphism represents an extreme crustal thermal event with peak conditions exceeding 900C at 7–13 kbar.In the modern-style plate tectonic system,records of the UHT metamorphism are relati...
supported by the National Natural Science Foundation of China(Grant Nos.41688103&42003026)。
The lower crust beneath the North China Craton(NCC)was transformed during the craton destruction in the Mesozoic,however,the transformation processes are yet to be fully understood.Compositional and geochronological v...
Until the middle of the 20th century,the continental crust was considered to be dominantly granitic.This hypothesis was revised after the Second World War when several new studies led to the realization that the conti...
funded by Foreign Expert grants to M.Santosh from the China University of Geosciences(Beijing)。
The Madurai Block in the Southern Granulite Terrane(SGT)of Peninsular India is one of the largest crustal blocks within the Neoproterozoic Gondwana assembly.This block is composed of three sub-blocks:the Neoarchean No...
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...
supported by the National Natural Science Foundation of China(Grant Nos.42072058,41772054,41572039)。
Monazite is an important accessory mineral in the pelitic granulites(Weihai area,Sulu orogen),and is also a powerful monitor for understanding the metamorphic evolution of the granulites.The pelitic granulites incongr...
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...