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1.- SANDSTONE-FILLED FLUVIAL CHANNEL IN INNTER-PLATFORM CARBONATES (URGONIAN LIMESTONES, CHAMBOTTE QUARRY, HAUTE-SAVOIE, FRANCE). EVIDENCE OF A TECTONICALLY INDUCED SEA-LEVEL CHANGE DURING THE EARLY APTIAN
 ALICANTE: UNIV. ALICANTE, 1998
15TH. INTERNATIONAL SEDIMENTOLOGICAL CONGRESS. ABSTRACTS
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