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1.- A NEW TYPE OF BEDFORM PRODUCED BY BACKFILLING PROCESSES IN A SUBMARINE CHANNEL, LATE MIOCENE, TABERNAS-SORBAS BASIN, SE SPAIN
SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS; TULSA, OK; USA; UNITED STATES, 2001
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2.- MAGNETIC CONSTRAINTS ON THE THERMAL EVOLUTION OF A COLLAPSING OROGEN
BLACKWELL SCIENCE FOR THE ROYAL ASTRONOMICAL SOCIETY, THE DEUTSCHE GEOPHYSIKALISCHE GESELLSCHAFT AND, 2002
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