Monitoring rapid temporal changes in a volcano with coda wave interferometry, Geophys

[1] Multiply–scattered waves typically dominate the late part of the seismic coda in local earthquake seismograms. Small medium changes that have no detectable influence on the first arrivals are amplified by multiple scattering and may thus be readily observed in the coda. We exploit this idea usin...

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Bibliographic Details
Main Authors: Er Grêt, Roel Snieder, Richard C. Aster, Philip R. Kyle
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2005
Subjects:
32
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.70.4321
http://www.mines.edu/~rsnieder/Erebus05.pdf