|2003 Seattle Annual Meeting (November 2–5, 2003)|
|Paper No. 66-9|
|Presentation Time: 10:45 AM-11:00 AM|
EARTHQUAKE-INDUCED FLUID PRESSURE CHANGES AT LONG VALLEY, CALIFORNIA: RESULTS FROM THE LONG VALLEY EXPLORATION WELL
ROELOFFS, Evelyn A.1, FARRAR, C.D.2, HENFLING, J.A.3, HOWLE, J.F.2, JACOBSON, R.D.3, and SNEED, M.4, (1) Western Earthquake Hazards Team, U.S. Geol Survey, 1300 SE Cardinal Court, Vancouver, WA 98683, firstname.lastname@example.org, (2) U.S. Geol Survey, Carnelian Bay, CA, (3) Geothermal Research Dept, Sandia National Laboratories, Albuquerque, NM, (4) U.S. Geol Survey, Sacramento, CA|
At Long Valley caldera, California, both local and distant earthquakes have produced persistent water level drops in wells on and north of the caldera’s resurgent dome, accompanied by earthquake-induced fluid level increases in the caldera’s hydrothermally active south moat.
Earthquake-induced water-level drops on and north of the resurgent dome may represent diffusion of localized fluid pressure drops induced abruptly by seismic waves. We evaluate this hypothesis using recent data from the Long Valley Exploration Well (LVEW), a 3 km deep borehole penetrating the center of the resurgent dome. The uncased interval of the LVEW penetrates relatively impermeable metapelite, and fluid communication is primarily through a conductive fracture 2.6 km below the surface. It has proven useful to collect data using pressure-temperature logging tools built to operate for extended periods at the depth of the fracture zone (temperature 102° C, pressure 22.3 MPa). Data from a pumping test in September, 2001, are consistent with a high-conductance planar fracture 10-100 m long in country rock with hydraulic diffusivity of 1-10 m2/s. Tidal amplitudes at the fracture zone depth are 1.93 kPa peak-to-peak, and the ratio of pressure change to strain based on the M2 earth tide constituent is 30.3 kPa/microstrain.
Both the Hector Mine, California (Oct. 16, 1999, M7.1) and Denali Fault, Alaska (Nov. 4, 2002, M7. 9) earthquakes produced steplike pressure drops in the LVEW which reached their minimum values (1.24 kPa and1.17 kPa, respectively) within 3 hours. In contrast, water level drops induced by the same two earthquakes at the shallower LKT well, 4 km NW of the center of the dome, required 10 to 15 days to reach their minima. The Denali Fault earthquake response at the LVEW was not only faster than at LKT, but also about twice as large, consistent with fluid pressure changes occurring abruptly with the passage of seismic waves at a location closer to the LVEW than to LKT. The pressure drops caused by the Hector Mine earthquake are less consistent with this conceptual model, because the fluid pressure dropped slightly more in LKT than in the LVEW. Continued fluid-pressure monitoring should yield more information about the time-space distribution of earthquake-induced fluid-pressure changes at Long Valley.
2003 Seattle Annual Meeting (November 2–5, 2003)
|Session No. 66|
M. King Hubbert at 100: The Enduring Contributions of Twentieth-Century Geology’s Renaissance Man
Washington State Convention and Trade Center: 602/603/604
8:00 AM-12:00 PM, Monday, November 3, 2003
Geological Society of America Abstracts with Programs, Vol. 35, No. 6, September 2003, p. 196
© Copyright 2003 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.