Jt. Rutledge et al., RESERVOIR CHARACTERIZATION USING OIL-PRODUCTION-INDUCED MICROSEISMICITY, CLINTON COUNTY, KENTUCKY, Tectonophysics, 289(1-3), 1998, pp. 129-152
Microseismic monitoring tests were conducted from 1993 to 1995 in the
Seventy-Six oil field, Clinton County, Kentucky. Oil is produced from
low-porosity, fractured carbonate rocks at <600 m depth. Downhole geop
hones were deployed in wells located within 120 to 250 m of new produc
tion wells. Three tests were conducted sequentially for 9.5-, 20.5-, a
nd 30-week periods during which 110, 180 and 3237 microearthquakes wer
e detected, respectively. Moment-derived magnitudes ranged from -2.5 t
o 0.9. Volumes extracted ranged from about 1300 to 1800 m(3); no injec
tion operations were conducted. Gross changes in production rate corre
late with event rate: event rate lags changes in production rate by 2
to 3 weeks. Hypocenters and first-motion data have revealed previously
undetected, low-angle thrust faults above and below the currently dra
ined depth intervals. Production history, well logs and drill tests in
dicate that the seismically active faults or fractures are previously
drained intervals that have subsequently recovered to hydrostatic pres
sure via brine invasion. Storage capacity computed for one of these dr
ained fractures implies that total oil production represents about 20%
of total pore volume. Correlation of older production intervals and w
ell-ion porosity anomalies with the seismically active faults indicate
that the oil reservoir in the study area is primarily a set df compar
tmentalized, low-angle thrust faults. Although low-angle fracture sets
have not previously been considered in the exploration and developmen
t of the area, the mapped thrust faults are consistent with other inve
stigators' interpretations of oil associated with secondary fracture s
ets occurring along deeper-seated, wrench-fault structures. Stress det
ermined from composite focal mechanisms indicates a near-surface (<550
m) thrust regime. Maximum horizontal stress direction is N15 degrees
W +/- 15 degrees, rotated approximately 90 degrees from regional orien
tation. The seismic behavior is consistent with poroelastic models tha
t predict slight increases in horizontal compressive stress above and
below currently drained volumes. Pressure re-equilibration via brine i
nvasion replacing previously produced oil along the seismically active
faults should also be weakly promoting the observed seismic failure.
Total estimated production-induced stress change promoting slip is app
roximately 0.02 MPa, (C) 1998 Elsevier Science B.V. All rights reserve
d.