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• W4306319032 endingPage "229607" @default.
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• W4306319032 abstract "During orogenesis, the forming structures vary according to several factors such as the nature of rocks, geological environment, P-T conditions, and type of collision. Deformational styles play a significant role in orogenic processes. While thin-skinned tectonics comprise only supracrustal deformation, in thick-skinned tectonics both supracrustal rocks and the basement are deformed reaching Moho depths. Both styles may coexist in a single orogenic system and the recognition of different sectors may help to unravel the nature of the orogen. In this paper, we apply the definition of tectonic styles to the São Miguel do Aleixo Shear Zone, a major transpressive shear zone in the Sergipano Belt, NE Brazil. It separates domains with different structural and metamorphic grades and provides evidence for understanding the tectonic implications of this structure and its role in the evolution of the orogen. We suggest that the São Miguel do Aleixo Shear Zone is a major crustal boundary formed during the oblique collision with and a possible transitional region between areas with dominant thin-skinned and thick-skinned tectonics. The presence of both tectonic styles together with metamorphic grade and geological environment lead to suggest that accretionary processes had a key role in the evolution of the Sergipano Belt. • Accretionary process in Western Gondwana revealed by aeromagnetic data. • Main suture zone at the southern limit of the Pernambuco-Alagoas Superterrane. • Aeromagnetic characterization of Sergipano Belt, Borborema Province, NE Brazil." @default.
• W4306319032 created "2022-10-16" @default.
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• W4306319032 date "2022-12-01" @default.
• W4306319032 modified "2023-09-26" @default.
• W4306319032 title "Oblique collision and accretionary processes in the South Borborema Province: Insights from structural geology and geophysical data" @default.
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• W4306319032 doi "https://doi.org/10.1016/j.tecto.2022.229607" @default.
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