T143 Structural Geology and Geomechanics in Applied Geosciences
Monday, 23 September 2019
1:30 PM - 5:30 PM
Room 231ABC, North Building
SCALE DEPENDENT VARIATIONS IN FRACTURE NETWORK PROPERTIES AND IMPLICATIONS FOR RESERVOIR CHARACTERIZATION: A FRACTURED CARBONATE ANALOGUE STUDY, NW MONTANA
Paper number: T143-2
Program: Technical Sessions
Time: 1:45 PM – 2:00 PM
Authors
-
Clare E. BondUniversity of Aberdeen, Aberdeen, N/A
-
Hannah WatkinsUniversity of Aberdeen, Aberdeen
-
Mark CooperSherwood GeoConsulting Inc, Calgary, AB
-
Mark CooperUniversity of Aberdeen, Aberdeen, N/A
-
Marian J. WarrenCalgary, AB
Abstract
Fracture orientations at the site are complex and variable, with six discrete fracture sets identified. Only two sets, oriented approximately parallel and perpendicular to the axial trace of the anticline, show evidence of a systematic increase in intensity with proximity to the fold hinge. We find that structural control on fracture intensity is subordinate to lithological control in that grainstone and packstone lithologies exhibit lower fracture intensities than fine-grained, mud-supported units in multiple structural positions across the anticline. Comparison of different observation scales and resolutions suggests that large-scale, low resolution data provide a better representation of structural controls on fracture occurrence, while small-scale, high-resolution data highlight the influence of lithology. Based on these results, we suggest that reservoir modelling strategies should focus on both downscaling from lower-resolution data and upscaling from isolated, high-resolution sample sites. This multi-scale approach will likely represent the most effective method for characterizing fractured carbonate reservoirs and predicting permeability pathways in structures of this type.
Geological Society of America Abstracts with Programs. Vol. 51, No. 5
doi: 10.1130/abs/2019AM-338778
© Copyright 2019 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.