Records of the accretionary, collisional and post-collisional evolution of western Gondwana in the high-grade core of the Araçuaí-Ribeira orogenic system, SE Brazil

• Published in: Precambrian research Vol. 397; p. 107191
• Main Authors: Santiago, Raíssa, Caxito, Fabricio de Andrade, Pedrosa-Soares, Antonio, Neves, Mirna Aparecida, Dantas, Elton Luiz, Calegari, Salomão Silva, Lana, Cristiano
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01-10-2023
• Subjects: Collisional orogen; Geochronology; Gondwana; Isotope geochemistry; Plate tectonics; Wilson cycle; Geochronology; Wilson cycle; Plate tectonics; Collisional orogen; Isotope geochemistry; Gondwana
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2023.107191

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•Pre-, syn-, and post-collisional plutons in a multi-intrusion batholithic system.•Juvenile Tonian island arc remnants preserved as roof pendants and mega-xenoliths.•Ediacaran pre-collisional tonalites/granodiorites as main bodies of the orogenic core.•Syn-collisional garnet-bearing leucogranites formed as crustal melts at 575–560 Ma.•Post-collisional undeformed A-type granites intruded at 500 Ma.
High-grade metamorphism, extensive partial melting, and polyphase deformation often obliterate records of pre-collisional stages in ancient orogens, making it hard to unravel Precambrian accretionary events. In western Gondwana, the high-grade core of the Araçuaí-Ribeira Orogenic System (AROS) comprises pre-collisional rock-assemblages largely disrupted, overprinted, and remelted by collisional and post-collisional tectono-metamorphic and igneous events, hampering reconstructions of its accretionary history. Detailed studies reveled remnants of an Early Tonian (860–840 Ma) island arc, forming km-size roof-pendants and mega-xenoliths within the composite Caxixe batholith, in the boundary zone between the Araçuaí and Ribeira orogens. We further characterize the Caxixe batholith and surrounding plutons, showing that the main stage of magmatism is composed of pre-collisional orthogneisses, partially migmatized and crystallized between ca. 607–580 Ma, thus, much later than the Tonian island arc records. Those Ediacaran granitic rocks represent intrusions of calc-alkaline magmas with elemental geochemistry and isotopic (εHf(t): −6 to −10, whole-rock εNd(t): −4.9 to −9.5, and 87Sr/86Sr(i): 0.706–0.711) data correlated with the continental-margin Rio Doce arc. This contrasts with signatures indicative of a mantle source εHf(t) = +10 to + 14, εNd(t) = +0.9 to + 6.4, and 87Sr/86Sr(i) = 0.698–0.704) of the Early Tonian arc remnants. Intruding the pre-collisional granitic plutons, garnet-bearing leucogranites dated at ca. 575 Ma and a mafic intrusion of ca. 560 Ma mark the transition from the syn-collisional to late-collisional stages. Post-collisional, non-deformed, A-type granites with the most evolved isotopic signatures (εHf(t): −22; εNd(t): −5.6 to −13.2) intruded at ca. 500 Ma, ending the long-lasting orogenic history documented in the region. Our results demonstrate that a basement composed of an early Tonian juvenile arc docked with a continental margin and hosted several intrusions of an early Ediacaran continental-margin magmatic arc that, in turn, were intruded by collisional and post-collisional magmas from the Late Ediacaran to Cambrian, finally forming the main plutonic masses of the Araçuaí-Ribeira Orogenic System (AROS) core, during the complex history of western Gondwana assembly.