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1.- Evolution of the late Pleistocene Mojanda-Fuya Fuya volcanic complex (Ecuador), by progressive adakitic involvement in mantle magma sources
Springer International [for the] International Association of Volcanology and Chemistry of the Earth, 2009
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2.- TRANSITION ENTRE MAGMATISMES CALCO-ALCALIN ET ADAKITIQUE DANS LE CAS D'UNE SUBDUCTION IMPLIQUANT UNE RIDE OCEANIQUE; LE VOLCAN CAYAMBE (EQUATEUR) ;TRANSITION FROM CALC-ALKALINE TO ADAKITIC MAGMATISM AT CAYAMBE VOLCANO, ECUADOR; THE INFLUENCE OF OCEANIC RIDGE SUBDUCTION
UNIVERSITE BLAISE PASCAL; CLERMONT-FERRAND; FRA; FRANCE, 2001
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