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1.- ARE THE REGIONAL VARIATIONS IN CENTRAL AMERICAN ARC LAVAS DUE TO DIFFERING BASALTIC VERSUS PERIDOTITIC SLAB SOURCES OF FLUIDS?
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2002
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2.- PETROLOGY OF TITANIAN CLINOHUMITE AND OLIVINE AT THE HIGH-PRESSURE BREAKDOWN OF ANTIGORITE SERPENTINITE TO CHLORITE HARZBURGITE (ALMIREZ MASSIF, S. SPAIN)
SPRINGER INTERNATIONAL; HEIDELBERG-NEW YORK; III; INTERNATIONAL, 2005
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