68th EAGE Conference and Exhibition Incorporating SPE EUROPEC 2006 2006
DOI: 10.3997/2214-4609.201402389
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A New Technique for Pressure - Saturation Separation from Time-Lapse Seismic - Schiehallion Case Study

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Cited by 10 publications
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“…The first step is to select a seismic attribute map that is sensitive to the reservoir changes. Examples of the range of possible seismic attributes suited for this purpose are given by Floricich et al (2006); however, it is known that the choice is field dependent. After selection, a discrete grid of points is then overlain on top of the attribute map, and across the fault segment of interest (figure 1).…”
Section: Fault Transmissibility Analysis Using 4d Seismic Datamentioning
confidence: 99%
“…The first step is to select a seismic attribute map that is sensitive to the reservoir changes. Examples of the range of possible seismic attributes suited for this purpose are given by Floricich et al (2006); however, it is known that the choice is field dependent. After selection, a discrete grid of points is then overlain on top of the attribute map, and across the fault segment of interest (figure 1).…”
Section: Fault Transmissibility Analysis Using 4d Seismic Datamentioning
confidence: 99%
“…Production started in 1998, and during the course of production, lack of support from injectors and a weak aquifer influx has led to a strong pressure decrease and a drop below the bubble point with the consequent liberation of free gas from the solution. The field is non-compacting (Floricich et al 2006) and segregated by a series of east-west trending normal faults, which divide the reservoir into five distinct segments with limited or no lateral communication. This character of the field enables us to select a single segment to act as a manageable data set for our study.…”
Section: Data For the Studymentioning
confidence: 99%
“…However the water saturation signal tends to dominate in this reservoir (Alvarez and MacBeth 2012) and the blue hardening persists -see wells I2, I3, I7 and I10 in the north, north-west and western portions of the segment. (between 1996-2002), of the sum of all negative amplitudes in a window defined from the top of T31a to the base of T31b (a known attribute for this field, see Floricich et al 2006). b) Geobodies in our case study that were achieved using seismic data.…”
Section: Data For the Studymentioning
confidence: 99%
“…The AVO impact was also investigated for North Sea field data ( Floricich et al . ; Alvarez and MacBeth ). Using another modified form of Landrø’s results, Trani et al .…”
Section: Introductionmentioning
confidence: 98%