Search Results - "Magalhães, Antonio J.C."
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Sedimentary petrology and detrital zircon U–Pb and Lu–Hf constraints of Mesoproterozoic intracratonic sequences in the Espinhaço Supergroup: Implications for the Archean and Proterozoic evolution of the São Francisco Craton
Published in Precambrian research (01-09-2015)“…•Continental to shallow marine siliciclastic deposits derived from recycled sources.•Primary sources were either related to collisional or rift tectonic…”
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Post‐Jurassic brittle deformation of Lusitanian Basin in the context of W Iberia evolution
Published in Basin research (01-12-2023)“…Abstract A detailed structural analysis of the fracture network exposed in the Jurassic strata is used to reconstruct the Lusitanian Basin's brittle tectonic…”
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Stratigraphic evolution from the early Albian to late Campanian of the Potiguar Basin, Northeast Brazil: An approach in seismic scale
Published in Basin research (01-10-2020)“…Five 3rd‐order depositional sequences are interpreted from the early Albian to late Campanian interval in the Potiguar Basin. An integrated analysis of seismic…”
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Middle Jurassic multi‐scale transgressive–regressive cycles: An example from the Lusitanian Basin
Published in The depositional record (01-02-2023)“…Multi‐scale transgressive–regressive cycles from the mid‐Jurassic were recognised in the Central Lusitanian Basin, Portugal. These cycles allow the…”
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Reply to the discussion and comments of Azerêdo et al. (2023) and Schneider et al. (2023) on the paper by Magalhães et al. ‘Middle Jurassic multi‐scale transgressive–regressive cycles: An example from the Lusitanian Basin’, The Depositional Record , 9, 174–202
Published in The depositional record (01-11-2023)“…Reply to the discussion and comments of Azerêdo et al. (2023) and Schneider et al. (2023)…”
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Age constraints on crystal-tuff from the Espinhaço Supergroup — Insight into the Paleoproterozoic to Mesoproterozoic intracratonic basin cycles of the Congo–São Francisco Craton
Published in Gondwana research (01-01-2015)“…The U–Pb data from the volcanic and detrital zircon grains of the Tombador Formation in Chapada Diamantina, Bahia, provide the depositional age of the top of…”
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