supported by the National Natural Science Foundation of China(Grant Nos.41888101,41890834,91755213);the Most Special Fund(MSFGPMR02-3)from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan;a contribution to the IUGS International Lithosphere Program(2023-TF1)“Formation,Character,History and Behavior of Earth’s Oldest Lithospheres”。
Geological maps encode vast amounts of data about rock types,ages,chemistry,orogenic architecture and deep-time history or different tectonic units,yet these are often difficult to extract because of the way different...
financial support from the CNPq(National Council for Scientific and Technological Development)under grant 141707/2016-0 to Lorena Martins;financial support provided by CNPq awarded to Cristiano Lana。
Field observations and CA-LA-ICP-MS U–Pb zircon ages and Hf isotope compositions obtained from migmatitic orthogneisses and granitoids from the Belo Horizonte Complex,southern São Francisco Craton,indicate a major pe...
supported by the National Natural Science Foundation of China(grants No.41872194,41872203)
Objective Early Precambrian rocks are widely distributed in the khondalite series belt of the North China Craton(NCC),and previous studies have shown that the metamorphic ages of^2.5 Ga and^1.95 Ga are widespread.
supported by the CNPq/Universal Project(Grant No.485539/2012-8);the Instituto Nacional de Ciencia e Tecnologia de Geociencias da Amazonia(INCT/GEOCIAM; Grant No.610010/2009-3)
The southeastern Guyana Shield,northeast Amazonian Craton,in the north of Brazil,is part of a widespread orogenic belt developed during the Transamazonian orogenic cycle(2.26-1.95 Ga)that includes a large Archean cont...
the Science Foundation of China University of Petroleum,Beijing (2462017YJRC032);the Science Foundation of State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum,Beijing (PRP/indep-4-1702);the National Key Basic Research Program of China (No.2012CB416603);the National Natural Science Foundation of China (Grant Nos.41430207 and 90914001).
The Liaodong Peninsula,in the northeastern part of the Eastern Block in the North China Craton,China, consists of lithologic units from Archean to Cenozoic in age.The basement rocks consist of widespread amphibolite-t...
The Neo-Archean Sonakhan Greenstone Belt(SGB) located in the north-eastern fringes of Bastar craton,Central India, is dominated by Basalts, Andesites, Dacites and Rhyolites association. Partial melting modeling on the...
supported through the years by Innovation Fellowship funds of the National Research Foundation (Innovation Postdoctoral Fellowship grant number 80422);a Post-doctoral Fellowship of the University of Johannesburg (at UJ);SIEF funds(Grant No. RP04-063 at Curtin)to AA;the NRFNEP funded (grant#93208)LA-MC-ICPMS;CIMERA for their further financial support of the laboratory
In the Kaapvaal craton of southern Africa, as well as other Archaean cratons worldwide, the progression from dominant tonalite-trondhjemite-granodiorite(TTG) to granite-monzogranite-syenogranite(GMS)rock types is inte...
the Key Program of the Ministry of Land and Resources of China (121201102000150012,DD20160121-03, 121201102000150010-04,DD20160343-01);the National Natural Science Foundation of China (41172127,41472169).
The mainland of China is composed of the North China Craton,the South China Craton,the Tarim Craton and other young orogehie belts.Amongst the three cratons,the North China Craton has been studied most and noted for i...
supported by the John Elleman scholarship at the University of Cape Town through the African Earth Observatory Network(AEON) initiative;the Natural Environment Research Council, UK, grant number NE/H008276/1;the Scottish Universities Environmental Research Centre (SUERC)
Borehole and surface samples from the Archean Tanzania Craton were analysed for apatite fission track(AFT) and(U-Th)/He data with the aim of deciphering cooling histories of the basement rocks. Fission track dates fro...
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 ...