2007
DOI: 10.1190/1.2737119
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Seismic monitoring and geomechanics simulation

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Cited by 14 publications
(8 citation statements)
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“…Such an inversion contributes to the understanding of how fluids are moving (sweeping) through a reservoir, of levels of intercompartment pressure communication, and whether fluid is produced from locations away from the wells (Greaves and Fulp, 1987;Landrø, 2001;Lumley, 2001;Calvert, 2005;Hodgson et al, 2007;Wikel, 2008). Knowledge of reservoir pressure can also be used to estimate stress and strain variations outside the reservoir (Herwanger and Horne, 2005;Dusseault et al, 2007;Scott, 2007). Identifying those stress patterns helps to guide drilling decisions and reduce the cost of repairing or replacing wells snapped or sheared by high stresses.…”
Section: Introductionmentioning
confidence: 99%
“…Such an inversion contributes to the understanding of how fluids are moving (sweeping) through a reservoir, of levels of intercompartment pressure communication, and whether fluid is produced from locations away from the wells (Greaves and Fulp, 1987;Landrø, 2001;Lumley, 2001;Calvert, 2005;Hodgson et al, 2007;Wikel, 2008). Knowledge of reservoir pressure can also be used to estimate stress and strain variations outside the reservoir (Herwanger and Horne, 2005;Dusseault et al, 2007;Scott, 2007). Identifying those stress patterns helps to guide drilling decisions and reduce the cost of repairing or replacing wells snapped or sheared by high stresses.…”
Section: Introductionmentioning
confidence: 99%
“…Our approach to this is to define a zone surrounding the reservoir proper within which these diffusion processes act over the simulation time, and discretize this region coarsely with finite elements (e.g. Dusseault et al, 2007;Yin et al in press).…”
Section: Discussionmentioning
confidence: 99%
“…This allows an earth model to be assembled, and the geomechanics model will be based on the use of seismics to interpolate between wells. To avoid excessive model complexity, usually a limited number of GMUs are defined (6)(7)(8)(9)(10)(11)(12)(13)(14)(15)(16)(17)(18)(19)(20), and usually these are chosen to correspond as well with clear lithostratigraphic units. In each GMU, a set of identical mechanical and petrophysical parameters is usually stipulated (although stochastic simulation can be used to vary parameters to simulate heterogeneity at various scales).…”
Section: Seismics and The Geomechanics Whole Earth Modelmentioning
confidence: 99%