Isotopic and trace-element indications of lithospheric and asthenospheric components in Tertiary alkalic basalts, northeastern Brazil

Plate reconstructions at 30 Ma place northeastern Brazil over the Fernando de Noronha hotspot, presently similar to 250 km offshore northeastern Brazil. Tertiary basaltic centers in northeastern Brazil may therefore be products of the Fernando de Noronha hotspot. We examined alkalic basalt from seven similar to 30-13 Ma old centers in Rio Grande do Norte and Pernambuco states to assess this possible link. Compositions are primitive, where MgO concentrations range from 12.5 to 17 wt.%, and SiO2, from similar to 41 to 48 wt.%. Trace-element abundances and Sr. Nd, and Pb isotopic compositions compare well with those of ocean island basalt: Sr-87/Sr-86 = similar to 0.7038-0.7051, Nd-143/Nd-144 = similar to 0.51266-0.51280, and Pb-206/Pb-204 = similar to 18.52-19.35. There are correlations among SiO2-undersaturation, incompatible-element abundances, relative percentages of partial melting (based on La/Yb and La/Y ratios), and the degree of isotopic 'enrichment' inherited from mantle sources. There is also a negative correlation for La/Nb (similar to 0.6-0.86) vs. Ba/Nb (6.6-10.6), where lower La/Nb samples represent larger percentages of melting of a source comparatively enriched in radiogenic Sr. We attribute these compositional relationships to the lavas representing mixing of melts mainly from asthenosphere of largely HIMU plus DM characterization, probably the Fernando de Noronha plume, with melts from subcontinental lithosphere that was isotopically closer to EM1. Isotopic and trace-element compositions of the northeastern Brazil basalts are generally similar to those of Fernando de Noronha lavas (12-2 Ma), and some minor trace-element differences observed (e.g., more Zr, Nb, and less Th compared to northeastern Brazil basalts) are probably due to heterogeneity within the asthenospheric plume and to melt contributions from delaminated subcontinental lithosphere that may underlie Fernando de Noronha. (C) 1998 Elsevier Science B.V. All rights reserved.