Cordilleran Section - 101st Annual Meeting (April 29–May 1, 2005)
Paper No. 12-11
Presentation Time: 4:20 PM-4:40 PM

A GEOMECHANICALLY-BASED INVERSE METHOD FOR INTERPOLATING THE THREE-DIMENSIONAL STRESS FIELD IN A FAULTED RESERVOIR

FLODIN, Eric A.1, MAERTEN, Frantz2, and MAERTEN, Laurent2, (1) Geosciences, Indiana Univ-Purdue Univ Fort Wayne (IPFW), 2101 East Coliseum Blvd, Fort Wayne, IN 46805, flodine@ipfw.edu, (2) Igeoss, Cap Omega, Montpellier Cedex2, 34960, France

Information concerning the nature of the stress field in a reservoir is necessary for many oilfield applications, such as pre-drill wellpath planning and fault seal analysis. Available data usually include stress orientation and magnitude estimates of various quality along a limited number of wellbores. Current methods to map the reservoir volume stress field from these point and/or line data range from simplistic averaging to more sophisticated interpolation and geostatistical techniques. We present a new method to interpolate stress throughout a reservoir volume using a geomechanically-based numerical boundary element code, Poly3D, coupled with a weighted damped least-squares inverse solver. The primary advantage of this methodology over others is that the stress solution includes the effect of elastic interactions among faults. The code uses as input a 3D fault framework, with or without mapped displacements, and estimates of stress orientation and magnitude from wellbores, which can be weighted to data quality. Output is in the form of a ‘best-fit' remote stress field, which is in turn used to forward model the volumetric stress field. Results illustrating the utility of our tool are presented for a number of faulted reservoir scenarios.

Cordilleran Section - 101st Annual Meeting (April 29–May 1, 2005)
General Information for this Meeting
Session No. 12
Application of New Technologies to Petroleum Reservoirs: Implications for Exploration and Production
Fairmont Hotel: Crystal
1:15 PM-5:20 PM, Friday, April 29, 2005

Geological Society of America Abstracts with Programs, Vol. 37, No. 4, p. 51

© Copyright 2005 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.