supported by the National Natural Science Foundation of China (Grant Nos. 41630209, U2039203, 42130306)。
Cratons formed due to the specific melting regime of the primitive mantle with elevated mantle temperature during Archean.However,each craton has undergone a distinct evolution history,and some have lost their stabili...
Serpentinized rocks closely associated with Paleoproterozoic eclogitic metabasites were recently discovered at Eseka area in the northwestern edge of the Congo craton in southern Cameroon.Here,we present new field dat...
supported by Australian Research Council Linkage Grant No. LP130100722;the Geological Survey of Western Australia
Evidence for episodic crustal growth extending back to the Hadean has recently prompted a number of numerically based geodynamic models that incorporate cyclic changes from stagnant lid to mobile lid tectonics. A larg...
India has four Archean Cratons i.e.Bundelkhand,Bastar,Dharwar and Singhbhum.These four Cratons have a dense network of Archean to Proterozoic dykes cutting across the Archean crust.The systematic Geochronology
The Indian shield comprises a number of Archean–Paleoproterozoic cratonic blocks and predominantly Meso–Neoproterozoic mobile belts with Archean protoliths.All these ancient cratons were thought to be integral parts of
CSIR for Emeritus Scientist Scheme and to the Ministry of Earth Sciences for the project, MoES/PO(Seismo)/23(646)/2007
The Aravalli-Delhi and Satpura Mobile Belts (ADMB and SMB) and the Eastern Ghat Mobile Belt (EGMB) in India form major Proterozoic mobile belts with adjoining cratons and contemporary basins. The most convincing f...
supported by the Knowledge Innovation Program of the Chinese Academy of Sciences(Grant No.KZCX2-YW-Q08-3-4);the project from the State Key Laboratory for Mineral Deposits Research,Nanjing University(Grant No.15-09-08)
High-Mg (Mg#〉45) andesites (HMA) within cratons attract great attention from geologists. Their origin remains strongly debated. In order to examine and provide direct evidence for previous assumptions about HMA'...
Financial support over the last years was through Spanish MEC and MICINN grants CGL2005-02065/BTE and CGL2009-07984;UCM-Santander grant GR58/08;Argentinian grant 1728 AR PICT 1009
The role played by Paleoproterozoic cratons in southern South America from the Mesopro- terozoic to the Early Cambrian is reconsidered here. This period involved protracted continental amal- gamation that led to forma...
Neoarchean and Proterozoic sutures and collision zones are identified in the Indian Peninsular Shield based on high seismic velocity;gravity highs and high conductivity in the upper crust due to thrusting while sub- d...
Project supported by the National Natural Science Foundation of China (Grant Nos. 49572140, 49302035 and 49132970).
The tectonic analysis with regional geology of North China Craton (NCC) indicates that granulite facies province (GFP) located between northern marginal mobile belt (NMMB) and Archean craton represents the most import...