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1.- THE DEEP STRUCTURE OF NON-VOLCANIC RIFTED CONTINENTAL MARGINS ROYAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 1999 RESPONSE OF THE EARTH'S LITHOSPHERE TO EXTENSION Ver registro
2.- THE ROLE OF SYN-RIFT MAGMATISM IN THE RIFT-TO-DRIFT EVOLUTION OF THE WEST IBERIA CONTINENTAL MARGIN; GEOPHYSICAL OBSERVATIONS GEOLOGICAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 2001 NON-VOLCANIC RIFTING OF CONTINENTAL MARGINS; A COMPARISON OF EVIDENCE FROM LAND AND SEA Ver registro
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