HR: 0800h
AN: S51B-0150 [Abstracts]
TI: Seismic Noise Correlation with Seismicity and Fluid Flow
AU: * Dorman, L M
EM: ldorman@ucsd.edu
AF: Scripps Institution of Oceanography, UCSD, 9500 Gilman Drive, La Jolla, CA 92093-0220
United States
AU: DeShon, H R
EM: hdeshon@emerald.ucsc.edu
AF: Earth Sciences Department,
University of California, Santa Cruz, 1156 High St., Santa Cruz, CA 95064
United States
AU: Brown, K
EM: kmbrown@ucsd.edu
AF: Scripps Institution of Oceanography, UCSD, 9500 Gilman Drive, La Jolla, CA 92093-0220
United States
AU: Schwartz, S
EM: sschwartz@ucsc.earthsci.ucsd.edu
AF: Earth Sciences Department,
University of California, Santa Cruz, 1156 High St., Santa Cruz, CA 95064
United States
AU: Tryon, M
EM: mtryon@ucsd.edu
AF: Scripps Institution of Oceanography, UCSD, 9500 Gilman Drive, La Jolla, CA 92093-0220
United States
AB:
During the Costa Rica Seismic Zone Experiment (CRSEIZE), we observed
intriguing correlations between earthquake activity, seismic noise
observed on the seafloor, and fluid flow through the seafloor (K. M.
Brown and others, this meeting). These correlations are observed on
instruments separated by as much as 30 kilometers. Here we describe
the nature of the noise, the temporal patterns, and speculate about
the transmission mechanism and the source(s).
Seismic noise on the seafloor is strongly influenced by ocean wave
activity, so we first compare the temporal variations in noise with the
ocean wave field as computed from the global wind field by Tolman.
This comparison shows that the long-term (months) pattern of wave data
provides a baseline for the the seismic noise field, but does not
predict the shorter (days) impulsive noise anomalies which correlate
with variations in fluid flow.
At some sites, the noise shows spectral peaks which have been explained
as peaks in the mode Q of Scholte waves (Schreiner and Dorman) and
shear resonances (Godin and Chapman). The frequencies of these peaks
is controlled by the shear velocity structure and the frequencies
themselves provide earth data constraining the seafloor velocity
structure.
DE: 7209 Earthquake dynamics and mechanics
SC: Seismology [S]
MN: 2004 AGU Fall Meeting