Geology and Petrology of Metavolcanic Rocks in the
Neoarchean Mundo Novo Greenstone Belt, Eastern
São Francisco Craton, NE Brazil: Tectonic Setting
Considerations
Volume 1 - Issue 1
Ricardo Ramos Spreafico1* ,Johildo Salomão Figueiredo Barbosa1, Antônio Marcos Vitória de Moraes2 and
Francisco Dias de Souza Júnior2
- 1Institute of Geosciences, Federal University of Bahia, Brazil
- 2Mining Company of Bahia State, Brazil
Received: October 29, 2019 Published: November 12, 2019
Corresponding author: Ricardo Ramos Spreafico, Mining Company of Bahia State and Institute of Geosciences, Federal University
of Bahia, Brazil
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Abstract
Field and petrological data of metakomatiite, eastern and western metabasalts and metadacite were used to propose an
intraoceanic or intracontinental provenance for the Neoarchean Mundo Novo Greenstone Belt (MNGB), eastern São Francisco
Craton. Despite deformation, the metakomatiite preserves the spinifex texture and the eastern metabasalt’s pillow lava structure.
The metavolcanics are recovered by an ocean floor lithological association composed of chemical metasedimentary rocks and the
western metabasalt hosts ocean floor hydrothermal alteration zones. The eastern metabasalt plots in the IAT and MORB fields
and western metabasalt is mainly in the MORB field in the Zr vs. Zr/Y diagram, suggesting nearby oceanic settings. Heterogeneous
crustal assimilation and metamorphism during the Rhyacian-Orosirian explain the mineralogical differences between the two
metabasalts. The metakomatiite and metabasalts feature a vector from the MORB-OIB array to the volcanic arc array in the Nb/Yb
vs. Th/Yb diagram, similar to the intraoceanic arc-basin system of the Archean greenstone belts. The average (La/Yb) N ratio of 8.87
for the metadacite indicates a crustal contamination in subducting oceanic crust. An intraoceanic provenance in arc-basin settings
and oceanic crust assimilations are proposed for the Neoarchean MNGB, which was posteriorly compressed between cratonic
blocks during the Rhyacian-Orosirian and lies in the Contendas-Jacobina Lineament.
Keywords: Mundo Novo Greenstone Belt; metavolcanic rocks; Intraoceanic Setting; Petrology; São Francisco Craton
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