| Registros del 1 al 10 de 15 encontrados |
 1.- 3D stratigraphic forward modelling for analysis and prediction of carbonate platform stratigraphies in exploration and production
Elsevier; Oxford; GBR; United Kingdom, 2008
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 2.- A facies model for internalites (internal wave deposits) on a gently sloping carbonate ramp (Upper Jurassic, Ricla, NE Spain)
Elsevier; Amsterdam; NLD; Netherlands, 2012
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 3.- Characterization and 3-D modelling of reef buildups and associated facies in a Kimmeridgian carbonate ramp system (Jabaloyas, eastern Spain) as analogue for the Middle East Arab D Formation
[varies]; [varies]; III; International, 2012
GEO 2012; the 10th Middle East geosciences conference and exhibition; abstracts
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 4.- Continuity and facies heterogeneities of shallow carbonate ramp cycles (Sinemurian, Lower Jurassic, north-east Spain)
Wiley-Blackwell; Oxford; GBR; United Kingdom, 2010
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 5.- FACIES ANALYSIS AND CORRELATION OF HIGH-ORDER SEQUENCES IN MIDDLE-OUTER RAMP SUCCESSIONS; VARIATIONS IN EXPORTED CARBONATE ON BASIN-WIDE (SUPER 13) C (SUB CARB) (KIMMERIDGIAN, NE SPAIN)
BLACKWELL; OXFORD; GBR; UNITED KINGDOM, 2005
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 6.- Facies heterogeneity at interwell-scale in a carbonate ramp, Upper Jurassic, NE Spain
Elsevier; Oxford; GBR; United Kingdom, 2013
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 7.- Facies models of a shallow-water carbonate ramp based on distribution of non-skeletal grains (Kimmeridgian, Spain)
Springer-Verlag GmbH; Erlangen; DEU; Germany, 2010
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 8.- FROM PLATFORM TO BASIN TO SWELL; ORBITAL CONTROL ON SEDIMENTARY SEQUENCES IN THE OXFORDIAN, SPAIN
BLACKWELL; OXFORD; GBR; UNITED KINGDOM, 2005
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 9.- High-resolution chemostratigraphic records from lower Pliensbachian belemnites; palaeoclimatic perturbations, organic facies and water mass exchange (Asturian Basin, northern Spain)
Elsevier; Amsterdam; NLD; Netherlands, 2012
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 10.- Inter-well scale heterogeneity in a Late Jurassic carbonate ramp
American Association of Petroleum Geologists and Society for Sedimentary Geology; Tulsa, OK; USA; Un, 2010
2010 AAPG annual convention & exhibition; abstracts volume
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