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Seismic imaging using microearthquakes induced by hydraulic fracturing

Journal Article · · Geophysics
;  [1]; ;  [2]
  1. Massachusetts Inst. of Tech., Cambridge, MA (United States). Dept. of Earth, Atmospheric, and Planetary Sciences
  2. Los Alamos National Lab., NM (United States)
Seismic imaging using microearthquakes induced by hydraulic fracturing produces a three-dimensional (3-D), S-wave velocity model of the fractured zone, improves the calculated locations of the microearthquakes, and may lead to better estimates of fracture-plane orientations, fracture density, and water flow paths. Such information is important for predicting the amount of heat energy that may be extracted from geothermal reservoir. A fractured zone was created at the Los Alamos Hot Dry Rock Reservoir in north-central New Mexico within otherwise impermeable basement rock by injecting 21,000 m{sup 3} of water into a borehole under high pressure at a depth of 3.5 km. Induced microearthquakes were observed using four borehole seismometers. The P-wave and S-wave arrival times have been inverted to find the 3-D velocity structures and the microearthquake locations and origin times. The inversion was implemented using the separation of parameters technique, and constraints were incorporated to require smooth velocity structures and to restrict the velocities within the fractured region to be less than or equal to the velocities of the unfractured basement rock.
Sponsoring Organization:
USDOE
DOE Contract Number:
W-7405-ENG-36; FG02-86ER13636
OSTI ID:
143791
Journal Information:
Geophysics, Journal Name: Geophysics Journal Issue: 1 Vol. 59; ISSN GPYSA7; ISSN 0016-8033
Country of Publication:
United States
Language:
English