Carmen Rosa Cubas Padilla, Francisco Hernán Reguera, Eumenio Ancochea Soto, José Luis Brandle Matesanz, María José Huertas Coronel
The Southern Volcanic Complex II consists mainly o( basalts wilh some lrachybasalls and basa/tic trachyandesites. Its lower sequence is formed by middle a/kaline rocks whilsl in lhe upper one only mildly all ali Hy+OI -normative rocks are found. The variations in composilion are largely expfainec/ by similar C1ystal fractionation mode/s far both the lower and the upper sequence5. The varialion among different basa/tic types is due to different extraction rales of about 10-15¾, olivine being lhe dominanl phase, followed, in a lesser proportion, by clinopyroxene. The differencc bclwccn thc most diffcrcntialcc/ basalts and trachybasa/ts or basa/tic trachyandesiles could be explainec/ by exlraction o( clominanl clinopyroxene wilh pfagioc/ase and Fe-Ti oxides.
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