Evolução petrogenética e tectônica do evento Cariris Velhos na região de Afogados da Ingazeira (PE), terreno Alto Pajeú, Província Borborema

Abstract

The Tonian Cariris Velhos event was studied in the area around Afogados da Ingazeira town, Pernambuco State, Northeast Brazil, which is situated within the Alto Pajeú terrane, a Tonian-Ediacaran composite domain of the Borborema Province. The exposed rocks belong to the São Caetano Complex, which is formed of biotite-muscovite paragneisses and quartz-feldspathic gneisses, derived from arkosic or felsic volcanic protoliths, with marble and quartzite intercalations. The deformation started with a D1/D2 thrusting episode, when metamorphism ranged from greenschist to amphibolite facies, and was accompanied by emplacement of orthogneiss sheets. The subsequent episode, the D3 phase, had an extensional character and was marked by intrusion of small metadiorite dikes, which were strongly transposed by the D4 phase, a new episode of transcurrent deformation. The main structure of the D4 phase is the Afogados da Ingazeira shear zone (ZCAI), which Ediacaran age was well constrained by the associated Solidão granite, dating from 574 ± 54 Ma. A geochemical study of the metasedimentary rocks shows that the protoliths of the paragneisses located in the southeastern part of the ZCAI are greywackes, whereas those of the northwestern part are greywackes, lithic sandstones and arkoses, although the REE patterns of these samples normalized to NASC (North American Shale Composite) show minor differences between them. These metasedimentary rocks have geochemical signatures and patterns of synorogenic sediments compatible with island and continental arc sources. The geochemical patterns of the orthogneisses are also consistent with a magmatic arc environment, the same conclusion reached by other authors with respect to the metavolcanic rocks of the Alto Pajeú terrane. The occurrence of the pre-transcurrent D3 extensional episode suggests that the D1/D2 thrusting deformation and associated metamorphism may be related to orogenic processes, pointing to the existence of the Cariris Velhos orogeny.