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Early Cretaceous tholeiites of the Kwanza basin, western Angola, 300<space>km South of Luanda, are evolved basalts to basaltic andesites, characterized by low TiO 2 (<2 wt%) and incompatible element contents. Their petrographical, major and trace element and Sr-isotopic (0.70448-0.70752) compositions are similar to those of tholeiites of the Parana-Etendeka flood basalt province,...
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