References of "Cerepi, Adrian"
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See detailSedimentary and diagenetic processes related to mid-Paleocene exposure surface, effects on the carbonate reservoir properties: Southeastern Pyrenean carbonate platform, Spain
Loisy, Corinne; Cerepi, Adrian; Da Silva, Anne-Christine ULg et al

in 13ème congrès Français de Sédimentologie, Dijon. Livre des résumés, 2011 (2011)

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See detailStructural and environmental influence on the Causses dolomitized body (south-east France) and reservoir properties
Da Silva, Anne-Christine ULg; Cerepi, Adrian; Loisy, Corinne et al

in 14th Bathurst meeting, Bristol University, Abstract book (2011)

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See detailEtude comparative des modèles sédimentaires et diagénétiques entre les versants nord et sud des Pyrénéens de la plate-forme carbonatée du Paléocène moyen.
Loisy, Corinne; Cerepi, Adrian; Da Silva, Anne-Christine ULg et al

in 12e Congrès Français de Sédimentologie – Rennes 2009 – Livre des résumés, Publ. ASF, n°64 (2009)

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See detailcontribution to understanding of sedimentological and diagenetic processus related to a major emersive surface : example of the middle paleocene unconformity (MPU).
Loisy, Corinne; Kiefer-Ollier, Eloise; Cerepi, Adrian et al

in Book of Abstracts - 26th IAS meeting, Alghero, Sardenia (2009)

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See detailVariations in stratigraphic and reservoir properties adjacent to the Mid-Paleocene sequence boundary, Campo section, Pyrenees, Spain
Da Silva, Anne-Christine ULg; Loisy, Corinne; Cerepi, Adrian et al

in Sedimentary Geology (2009), 219

The Paleocene of the Campo section, Spain has different sedimentological characteristics above and below the Mid-Paleocene Unconformity. Beneath the unconformity sediments are dominated by evaporitic ... [more ▼]

The Paleocene of the Campo section, Spain has different sedimentological characteristics above and below the Mid-Paleocene Unconformity. Beneath the unconformity sediments are dominated by evaporitic carbonates and collapse breccias. Above it they are characterized by continental detrital beds alternating with paleosols. Different subaerial features are observed and correspond to different porosity values, pore–throat sizes and micrite morphologies. Unexposed or intertidal facies have low porosity, low throat–pore size (mesoporosity) and well preserved rhombic crystals. Intermediate exposed facies (paleosols) possess medium porosity, medium pore–throat size (microporosity) and mainly micro-rhombic crystals. Finally, the facies corresponding to high exposure intensity and to evaporitic original facies presents high porosity, permeability, large pore–throat size and rounded micritic crystals. These observations show that the emersion phase caused important dissolution, especially when associated with an easily dissolved original lithofacies. [less ▲]

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See detailContribution to understanding of sedimentological and diagenetic processus related to major emersive surfaces and their spatial variation
Loisy, Corinne; Da Silva, Anne-Christine ULg; Kieffer, Eloise et al

in Book of Abstracts - 25th meeting of the IAS, Patras, Greece (2007)

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See detail) Relationship between subaerial exposure features on a carbonate platform and reservoir properties (example of the Campo section, Spain, Paleocene).
Da Silva, Anne-Christine ULg; Loisy, Corinne; Cerepi, Adrian et al

in Abstract book 17th ISC - Fukuoka, Japan - 2006 (2006)

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See detailSubaerial exposure recording on a Paleocene carbonate platform – Example of the Campo section, Spain
Da Silva, Anne-Christine ULg; Loisy, Corinne; Toullec, Renaud et al

Conference (2006)

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See detailPaléoémersions : processus sédimentaires et diagénétiques associés
Loisy, Corinne; Da Silva, Anne-Christine ULg; Toullec, Renaud et al

in 10ème congrès français de sédimentologie - livret des résumés (2005)

Detailed reference viewed: 12 (4 ULg)