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Control of inherited structural fabric on the development and exhumation of passive margins-Insights from the AraçuaíOrogen(Brazil)

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Geoscience Frontiers 2023年第6期14卷 30-48页

作者： Ana Fonseca Tiago Novo Tobias Fonte-Boa Matheus Kuchenbecker daniel Galvão Carnier Fragoso daniel peifer Antônio Carlos Pedrosa-Soares Johan De Grave Laboratory for Mineralogy and Petrology Department of GeologyGhent UniversityKrijgslaan 281 S89000 GhentBelgium Universidade Federal de Minas Gerais Programa de Pós-Graduação em GeologiaCPMTC-IGCCampus PampulhaBelo HorizonteMGBrazil Centro de Pesquisas Professor Manoel Teixeira da Costa Instituto de GeociênciasUniversidade Federal de Minas GeraisBelo HorizonteBrazil Universidade Federal dos Vales do Jequitinhonha e Mucuri Instituto de Ciência e TecnologiaCentro de Estudos em GeociênciasLaboratório de Estudos TectônicosDiamantinaBrazil Petrobras Rio de JaneiroRJBrazil Instituto de Geociências Universidade Federal do Rio Grande do SulPorto AlegreRSBrazil Department of Geosciences University of TübingenSchnarrenbergstr.94-9672076 TübingenGermany

The AraçuaíOrogen,in eastern Brazil,was formed during the Neoproterozoic–Cambrian amalgamation of West *** the Mesozoic–Cenozoic opening of the South Atlantic Ocean,and the associated divergent tectonics,the orogen developed as basement to the passive margin of South America and was progressively covered by thick offshore sedimentary basins,particularly the Espírito Santo,Mucuri,and Cumuruxatiba basins,in which hydrocarbon systems have been *** understanding of the AraçuaíOrogen’s passive margin evolution,erosion,and sediment transfer to these basins ultimately depends on constraining the onshore exhumation in response to Mesozoic–Cenozoic ***,new and previously published data from apatite fission-track(AFT)analyses and inverse thermal history modelling of(Pre)Cambrian basement rocks from the AraçuaíOrogen resolve three discrete basement cooling and associated erosional exhumation *** the Pre-Rift phase,Jurassic–Hauterivian erosion of the AraçuaíOrogen is most likely related to the adjoining intra-continental West Gondwana flexural subsidence,which increased hillslope and river erosion *** the Rift and Transitional phases,Barremian–Albian accelerated phase of erosion is associated with the uplift of the Atlantic rift shoulders and the establishment of an oceanic *** the Drift phase,reactivations in response to far-field stresses likely triggered a Late Cretaceous–Paleocene rapid erosion *** rates at which these events unfolded vary spatially and are controlled by inherited *** AraçuaíOrogen experienced slower denudation rates in areas closer to the São Francisco Craton,which suggests that the tectonic reactivation and related surface uplift during the Mesozoic–Cenozoic is in first-order controlled by lithospheric ***,the structural framework of the Paramirim and Pirapora aulacogens and NE-oriented shear zones in the orogen’s southeast facilitated later *** the spati

关键词： Thermal history Denudation Tectonic inheritance Reactivations South Atlantic Hydrocarbons

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