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Cenozoic basalts carrying ultramafic mantlexenoliths occur in the Matilde, León and Chenque hillsin the Paso de Indios region, Argentina. The mantle xenolithsfrom the Chenque and León hills mainly presentporphyroclastic textures, whereas the Matilde hill xenolithshave coarse-grained to porphyroclastic textures. Theequilibrium temperatures are in the range of 780 to 940ºC,indicating a provenance from shallow sectors of the lithosphericmantle column that were subjected to a relativelylow heat ffiux at Cenozoic Era.

Short-scale variability of the SCLM beneath the extra-Andeanback-arc (Paso de Indios, Argentina): Evidence from spinel-faciesmantle xenoliths