Engineering properties of chalk related to diagenetic variations of upper cretaceous onshore and offshore chalk in the North Sea area (Record no. 171107)

MARC details
000 -LEADER
fixed length control field 02540nab a2200193 4500
008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL
Campo de control de longitud fija 260224s2009 xxu
245 00 - TITULO
Título Engineering properties of chalk related to diagenetic variations of upper cretaceous onshore and offshore chalk in the North Sea area
260 ## - PUBLICACION, DISTRIBUCION, ETC
Lugar de publicación, distribución, etc.
Nombre de publicador, distribuidor, etc.
Fecha de publicación, distribución, etc. oct. 2009
270 ## - FECHA DE CARGA
Fecha de carga 16/06/2010 ; 16/06/2010
300 ## - DESCRIPCION FISICA
Otra extensión 20 p. ; 151-170
520 ## - RESUMEN, ETC
Resumen Transcripción del resumen del autor. Predicting properties of reservoir chalk involve testing and modelling of easily obtainable outcrop chalk. However, variations in onshore and offshore chalk properties will expectedly occur due to different diagenetic history. Understanding diagenetic mechanisms and their consequences are thus a key issue when reservoir chalk characterization is based on outcrop chalk. In chalk of the Valhall field high pore pressure and hydrocarbon presence have counteracted recrystallization and cementation and preserved high porosity despite a burial depth of c. 3 km. As a consequence inter-particle connections are poorly developed and Valhall chalk is expectedly geomechanically weak. Similar high porosity and weak consolidation were observed in Danish outcrop chalk which expectedly will match the Valhall samples geomechanically. In chalk of the Dan, South Arne and Ekofisk fields recrystallization and cementation features are significantly better developed compared to the Valhall field. Calcite redistribution has strengthened particle contacts and reduced porosity, assumingly providing a geomechanically stronger chalk. Similar low porosity and well-developed recrystallization and cementation features are found in English chalk which from a geomechanical point of view may share characteristics with chalk of the Dan, South Arne and Ekofisk fields. Matrix permeability is related not only to porosity but also to specific surface area of chalk which is controlled partly by calcite recrystallization partly by type and amount of non-carbonate minerals. In onshore chalk significant mineralogical differences are reflected in varying specific surface area. In contrast, specific surface area of Upper Cretaceous reservoir chalk show little variation indicating that care must be taken when choosing an outcrop chalk as substitute for reservoir chalk during flooding experiments.
581 ## - ESTADO DE COLECCIÓN
Estado de colección 3-4
773 0# - CORRECCIÓN
Título Journal of Petroleum Science & Engineering
Partes relacionadas 68
942 ## - DESC. DE MATERIAL
Tipo de item KOHA Artículo de Revista
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Hjuler, M.L.
9 (RLIN) 42842
100 1# - RESPONSABLE PERSONAL
Apellido, Nombre Fabricius, I.L.
9 (RLIN) 42843
Holdings
Biblioteca propietaria Biblioteca actual Fecha de adquisición Inventario Total de préstamos Inventario Fecha de carga Tipo de item KOHA
Biblioteca Alejandro Angel Bulgheroni Biblioteca Alejandro Angel Bulgheroni 05/03/2026 200045965   200045965 05/03/2026 Artículo de Revista


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