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Characterization of fractures and faults: a multi‐component passive microseismic study from the Ekofisk reservoir
Author(s) -
Jones G.A.,
Kendall J.M.,
Bastow I.,
Raymer D.G.,
Wuestefeld A.
Publication year - 2014
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1111/1365-2478.12139
Subject(s) - microseism , geology , shear wave splitting , seismology , tectonics , fracture (geology) , economic geology , geothermal gradient , petrology , anisotropy , seismic anisotropy , passive seismic , shear (geology) , gemology , fault (geology) , regional geology , environmental geology , geophysics , engineering geology , geotechnical engineering , volcanism , physics , quantum mechanics , mantle (geology)
Fractures and faults within a reservoir can provide important pathways for the movement of reservoir fluids. Understanding the character and properties of these features on a range of length scales can be vital for the efficient exploitation of natural resources, whether it be enhanced oil and gas recovery, the safe storage of CO 2 , or better exploitation of geothermal heat. The monitoring of microseismicity within a reservoir illuminates active faults, but these events can be also used to characterize fracture networks through measurements of seismic anisotropy. In this study we use microseismic data acquired over an 18‐day period in April 1997 at the Ekofisk oil field in the North Sea. Using the analysis of seismic multiplets we delineate a number of sub‐vertical tectonic faults, which are consistent with previous core data analysis and seismic reflection work. We use shear wave splitting measurements, which are indicative of fracture‐induced seismic anisotropy, to infer the orientation of aligned aseismic fracture sets within the reservoir. The estimated fracture dip and strike from the shear wave splitting analysis are consistent with the active tectonic fractures characterized by the multiplets, but this analysis also illuminates spatial variations in fracture properties. Such monitoring on a longer term and with multiple wells is a promising tool for better understanding fracture and fault‐controlled flow within reservoirs.