European 3-D Reservoir Modelling Conference 1996
DOI: 10.2118/35487-ms
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Application of Seismic Data and Sequence Stratigraphy for Constraining a Stochastic Model of Calcite Cementation

Abstract: Copyr!ghl 1996 Souety 01 Petroleum Englneets Tfus papr was prepared Ior presentatum at the EuroPan 3-D Resewo(r Modellmg Conference held tinSIavanger Noruay, 16-17 F.@ 19S6 Th!s paper was selected for presentatwn by the SPE Prcgram Commrttes following rwvlew o! Information conlamed m an abstrOct submlfted by the author(s) Conlenls of the paper as presented, have not been rWBWd by the Society of PekOleum Engineers and are sublect to correc!aon by the author(s) The mater,al, aspresented, doss not necesswfy relle… Show more

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“…The calcite cemented layers can be identified in cores, wireline logs and analogous outcrops (Lien et al 1992;Evensen et al 1993;Gibbons et al 1993), and are interpreted to vary in lateral extent from discontinuous nodules to laterally extensive stratified layers that can be correlated between wells (see, for example, Figure 11 in Gibbons et al 1993). In addition, dipping reflectors of low to high amplitude are observed in seismic crosssections and time slices across the Sognefjord Formation, which are interpreted as clinoform surfaces associated with calcite-cemented concretions (Bakke et al 1996;Dreyer et al 2005;Holgate et al in review). Calcite cementation is therefore interpreted to occur preferentially along the flooding surfaces that bound the parasequences, and along clinoform surfaces within each parasequence.…”
Section: Geologic Context and Production History Of Reservoir Case Studymentioning
confidence: 99%
“…The calcite cemented layers can be identified in cores, wireline logs and analogous outcrops (Lien et al 1992;Evensen et al 1993;Gibbons et al 1993), and are interpreted to vary in lateral extent from discontinuous nodules to laterally extensive stratified layers that can be correlated between wells (see, for example, Figure 11 in Gibbons et al 1993). In addition, dipping reflectors of low to high amplitude are observed in seismic crosssections and time slices across the Sognefjord Formation, which are interpreted as clinoform surfaces associated with calcite-cemented concretions (Bakke et al 1996;Dreyer et al 2005;Holgate et al in review). Calcite cementation is therefore interpreted to occur preferentially along the flooding surfaces that bound the parasequences, and along clinoform surfaces within each parasequence.…”
Section: Geologic Context and Production History Of Reservoir Case Studymentioning
confidence: 99%