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1.- MICROGRANULAR ENCLAVES AS EVIDENCE OF RAPID COOLING IN GRANITOID ROCKS; THE CASE OF THE LOS PEDROCHES GRANODIORITE, IBERIAN MASSIF, SPAIN
SPRINGER INTERNATIONAL; HEIDELBERG-NEW YORK; III; INTERNATIONAL, 2005
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2.- SR-ND ISOTOPIC RECORD OF MULTI-STAGE INTERACTIONS BETWEEN MANTLE-DERIVED MAGMAS AND CRUSTAL COMPONENTS IN A COLLISION CONTEXT; THE ULTRAMAFIC-GRANITOID ASSOCIATION FROM VIVERO (HERCYNIAN BELT, NW SPAIN)
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 1996
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3.- TWO-STAGE GRANITOID-FORMING EVENT FROM AN ISOTOPICALLY HOMOGENEOUS CRUSTAL SOURCE; THE LOS PEDROCHES BATHOLITH, IBERIAN MASSIF, SPAIN
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1999
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