| Registros del 1 al 6 de 6 encontrados |
1.- Contrasting deglacial sedimentary architecture along paleofjord systems due to distance to open-sea, and its importance for hydrocarbon generation; Late Carboniferous units of W-Gondwana, Argentina
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2009
European Geosciences Union general assembly 2009
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2.- FLOW PROCESSES IN MEANDERING SUBMARINE CHANNEL BENDS
 ALICANTE: UNIV. ALICANTE, 1998
15TH. INTERNATIONAL SEDIMENTOLOGICAL CONGRESS. ABSTRACTS
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3.- Mass-transport and relative sea level change in a Carboniferous deglacial succession; Jejenes Fm, Quebrada las Lajas, San Juan, Argentina
American Geophysical Union; Washington, DC; USA; United States, 2004
AGU 2004 fall meeting
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4.- SEDIMENT BYPASSING BY SANDY TURBIDITY CURRENTS: THE CONTROL OF FLOW CONCENTRATION ON GRAIN-SIZE BREAKS AND DUNE FORMATION
ALICANTE: UNIV. ALICANTE, 1998
15TH. INTERNATIONAL SEDIMENTOLOGICAL CONGRESS. ABSTRACTS
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5.- SLUMPS, DEBRIS FLOWS AND SANDY DEEP-WATER CHANNEL SYSTEMS; IMPLICATIONS FOR THE APPLICATION OF SEQUENCE STRATIGRAPHY TO DEEP WATER CLASTIC SEDIMENTS
GEOLOGICAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 1998
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6.- Submarine flow discharge changes as a way to explain incission-overspilling and other cycles in submarine channel sequences
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2009
European Geosciences Union general assembly 2009
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