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The generation and evolution of the Archean continental crust:The granitoid story in southeastern Brazil

Geoscience Frontiers 2022年第4期13卷 144-164页

作者： Rodrigo S.Marimon Chris J.Hawkesworth Elton L.Dantas Rudolph A.J.Trouw Wilson Teixeira Peter C.Hackspacher allen fetter Ciro A.Ávila Silvia Volante Atlas V.Corrêa Neto Everton M.Bongiolo Rodrigo Vinagre Maurício Simon Depto.de Geologia IGEOUniversidade Federal do Rio de JaneiroUFRJRio de JaneiroRJBrazil School of Earth Sciences University of BristolBristolUnited Kingdom Instituto de Geociências Universidade de BrasíliaUnBBrasíliaDFBrazil Instituto de Geociências Universidade de São PauloUSPSão PauloSPBrazil Instituto de Geociências e Ciências Exatas Universidade Estadual PaulistaRio ClaroSPBrazil Institute of Geology Mineralogy and GeophysicsRuhr-Universität BochumUniversitätsstraße 15044801 BochumGermany ISOTOPIA Lab School of EarthAtmosphere and EnvironmentMonash UniversityWellington RdClaytonVIC 3800Australia Programa de Pós-Graduação em Geociências IGUniversidade Federal do Rio Grande do SulUFRGSPorto AlegreRSBrazil

The Archean Eon was a time of geodynamic *** evidence of these transitions come from igneous/metaigneous rocks,which dominate cratonic segments *** data for granitoids from an Archean basement inlier related to the Southern S?o Francisco Craton(SSFC),are integrated with geochronological,isotopic and geochemical data on Archean granitoids from the *** rocks are divided into three main geochemical groups with different ages:(1)TTG(3.02–2.77 Ga);(2)mediumto high-K granitoids(2.85–2.72 Ga);and(3)A-type granites(2.7–2.6 Ga).The juvenile to chondritic(Hf-Nd isotopes)TTG were divided into two sub-groups,TTG 1(low-HREE)and 2(high-HREE),derived from partial melting of metamafic rocks similar to those from adjacent greenstone *** compositional diversity within the TTG is attributed to different pressures during partial melting,supported by a positive correlation of Dy/Yb and Sr/Zr,and batch melting *** proposed TTG sources are geochemically similar to basaltic rocks from modern island-arcs,indicating the presence of subduction processes concomitant with TTG ***~2.85 Ga to 2.70 Ga,the dominant rocks were K-rich *** are modeled as crustal melts of TTG,during regional metamorphism indicative of crustal *** compositional diversity is linked to:(i)differences in source composition;(ii)distinct melt fractions during partial melting;and(iii)different residual mineralogies reflecting varying P–T ***-collisional(~2.7–2.6 Ga)A-type granites reflect rifting in that they were closely followed by extension-related dyke swarms,and they are interpreted as differentiation or partial melting products of magmas derived from subduction-modified *** sequence of granitoid emplacement indicates subduction-related magmatism was followed by crustal thickening,regional metamorphism and crustal melting,and post-collisional extension,similar to that seen in younger Wilson *** is compelling evide

关键词： Granitoid petrogenesis Archean geodynamics Crustal evolution TTGs A-types Batch melting calculations

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