Neoarchean magmatism in the southeastern Amazonian Craton, Brazil: Petrography, geochemistry and tectonic significance of basalts from the Carajas Basin

The Neoarchean Carajas Basin is situated in the northern part of the Carajas Mineral Province. The main rock assemblages of this basin consist of volcano-sedimentary sequences composed predominantly of mafic volcanic rocks; and banded iron formations. The Grao-Para Group (GGP) is the dominant sequence in the basin. The basalts of Grao-Pard Group (Parauapebas Formation) are investigated using petrography, geochemistry and geochronology to decipher the nature and tectonic setting of the magmatism. These volcanic rocks occur in extensive succession of massive or amygdaloidal lava flows at least 370 m in thickness. The basalts are grayish green amygdaloidal, porphyritic, aphanitic or fine-grained, and hypocrystalline. The primary mineral assemblages consist predominantly of clinopyroxene and plagioclase. On the other hand, the secondary mineral assemblages consists mainly of chlorite, albite, Fe-epidote, quartz and calcite, and are interpreted as product of submarine hydrothermal alteration and/or sub-greenschist fades metamorphism. Geochemical investigations on volcanic rocks of the Parauapebas Formation show 51.12-55.26 wt% SiO2, 0.69-0.92 wt% TiO2, 7.02-12.35 wt % FeO, and MgO ranging from 4.38 to 7.38 wt%. Moreover, the rocks are sub-alkaline, plot in the transitional and calc-alkaline fields, and show either arc-like trace element patterns or similar to those of the upper continental crust. These features include LILE and LREE enrichment and Nb and Ti depletion. SHRIMP zircon U-Pb dating constrains the crystallization ages at 2749 +/- 6.5 and 2745 +/- 5 Ma (Early Neoarchean) regarding volcanic mafic rocks. Our data suggest that the basaltic rocks were derived from the subcontinental lithospheric mantle affected by upper continental crustal components. Although this volcanism could be originated by the opening of a back-arc continental basin, a rift setting is more plausible on the basis of regional geology. Thus, the Cara* Basin was likely formed in an extensional regime related to a rift setting at ca. 2.75 Ga. We propose that this rift basin is related to post-orogenic setting in the passage from the Mesoarchean to the Neoarchean. The rifting process could be associated to a slab breakoff and subsequent asthenosphere upwelling that provided heat for partial melting of the lithospheric mantle.