the Brazilian National Council for Scientific and Technological Development(CNPq)for financial support(grants 163459/2013-4 and 202267/2014-8 for G.S Teles and 305053/2014-0 for F.Chemale Jr.);the Australian Research Council(ARC)(grant DP140103393 for T.R.Ireland)。
Greenstone belts contain several clues about the evolutionary history of primitive Earth.Here,we describe the volcano-sedimentary rock association exposed along the eastern margin of the Gavião Block,named the Norther...
supported by the project of China Geological Survey(Grant No.DD20190438)。
The timing and mechanisms of lithospheric thinning and destruction of the North China Craton(NCC)remain controversial,and the overall geodynamics of the process are poorly understood.This paper documents Late Triassic...
The basement granite gneisses from the north-central Aravalli Craton in NW India were investigated for geochemistry and geochronology.In a peneplain terrain,the granite gneiss outcrops are scanty and samples were coll...
financially supported by the National Key Research and Development Program (Grant Nos. 2018YFC0603804);the China Geological Survey (Grants DD20190042, DD20190039 and DD20160048-05)
The early Mesozoic marked an important transition from collisional orogeny to post-orogenic extension at the northern margin of the North China Craton(NCC). In this study, we undertook zircon U-Pb dating and whole-roc...
Financial support for this study was jointly provided by the National Natural Science Foundation of China(Grant Nos.41421002and 41225008);MOST Special Fund from the State Key Laboratory of Continental Dynamics,Northwest University;Project for Key Innovative Research Team of Science and Technology in Shaanxi Province(Grant No.2013KCT-18)
The Helanshan tectonic belt(HTB) is a major tectonic divide between the Alxa and Ordos blocks in the North China Craton. The geochronology and petrogenesis of the mafic dykes in the northern HTB are keys to understand...
A precise U-Pb baddeleyite age of 1999±2 Ma has been obtained for the NNW trending Lac Shpogan dyke swarm of the James Bay area of the eastern Superior craton.Previously the age of the swarm was only
Supported by the National Natural Science Foundation of China (Grant No. 49832030).
Recent research on the tectonothermal evolution and geochronology in the Fuping, Hengshan and Wutaishan metamorphic complexes, together with the discoveries of a high-pressure granulite belt in the northern margin of ...