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Geological, geochemical and isotope diversity of similar to 134 Ma dykes from the Florianopolis Dyke Swarm, Parana Magmatic Province: Geodynamic controls on petrogenesis

Texto completo
Florisbal, L. M. [1] ; Janasi, V. A. [2] ; Bitencourt, M. F. [3] ; Nardi, L. V. S. [3] ; Marteleto, N. S. [2]
Número total de Autores: 5
Afiliação do(s) autor(es):
[1] Univ Fed Santa Catarina, Dept Geociencias, Ctr Filosofia & Ciencias Humanas, Campus Univ Trindade, BR-88010970 Florianopolis, SC - Brazil
[2] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP - Brazil
[3] Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Petrol & Geoquim, Av Bento Goncalves 9500, BR-91500000 Porto Alegre, RS - Brazil
Número total de Afiliações: 3
Tipo de documento: Artigo Científico
Fonte: JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH; v. 355, n. SI, p. 181-203, APR 15 2018.
Citações Web of Science: 0

The Florianopolis Dyke Swarm (FDS), one of the major dyke swarms belonging to the Early cretaceous (135-131 Ma) Parana Magmatic Province, is largely dominated by high Sr-Ti-P basalts that are confirmed here as feeders of the unique Urubici (=Khumib) lavas of the Parana and Edendeka lava piles on the basis of their age and geochemistry. Our study integrates field, petrographic, whole-rock geochemistry, and Sr-Nd-Pb isotope geochemistry of representative samples from three main areas of exposition (Santa Catarina Island, Garopaba and Pinheira beaches), thus encompassing the whole extension of the FDS. Compared to the Urubici lavas, the dykes have usually higher contents of LILE and LREE, more radiogenic Sr and Pb, and more unradiogenic Nd, features attributed to a more pronounced interaction with melts derived from the country rocks registered in the basic magmas that remained in the conduits. Some of these dykes show strongly interactive contacts that must be part of a wider zone of crustal melting, probably more developed at greater depths. Small volumes of intermediate to acidic rocks form the cores of some composite dykes, and correspond to products of fractional crystallization from Urubici basalts contaminated with high Rb/Sr, and U/Th crustal melts (probably derived from Neoproterozoic granites), as indicated by geochemical and Sr-Nd-Pb isotope data. The chemical and isotope signatures of the less contaminated FDS basalts and related Urubici lavas do not show clear evidence of inputs from primitive mantle, and seem heavily influenced by enriched mantle. This suggests that the mantle wedge that was affected by subduction during the Neoproterozoic may have been frozen and coupled to the base of the litho spheric plate where the Early cretaceous magmatism occurred. A control of previous tectonic limits on the sources of the Urubici basalts seems evident, since they seem to be related to the younger lithosphere from the South Domain, related to the Florianopolis Batholith, and no influence from the older ``cratonic{''} lithosphere of the Central Domain can be identified in their feeders. (C) 2017 Elsevier B.V. All rights reserved. (AU)

Processo FAPESP: 11/09673-2 - Idade, duração e significado tectônico do Enxame de Diques de Florianópolis, Província Magmática Paraná-Etendeka, a partir da combinação de estudos petrológicos e datações U-Pb em badeleíta e zircão
Beneficiário:Luana Moreira Florisbal
Linha de fomento: Bolsas no Brasil - Pós-Doutorado
Processo FAPESP: 12/06082-6 - A província magmática Paraná-Etendeka no Brasil: relações temporais e petrológicas entre o magmatismo toleítico e alcalino e suas implicações geodinâmicas
Beneficiário:Excelso Ruberti
Linha de fomento: Auxílio à Pesquisa - Temático