Evidence for non-constant energy/moment scaling from coda-derived source spectra

scientific article published in 2005

Evidence for non-constant energy/moment scaling from coda-derived source spectra is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2005GeoRL..3210306M
P356DOI10.1029/2005GL022405

P50authorWilliam R. WalterQ60728720
P2093author name stringAbraham Hofstetter
Rengin Gök
Kevin Mayeda
P2860cites workGlobal patterns of radiated seismic energy and apparent stressQ56386193
Observations of Earthquake Source Parameters at 2 km Depth in the Long Valley Caldera, Eastern CaliforniaQ57866619
Estimating Absolute Site EffectsQ57870086
Earthquake source scaling relationships from −1 to 5 ML using seismograms recorded at 2.5-km depthQ60701344
Does apparent stress vary with earthquake size?Q60715243
Regional Estimates of Radiated Seismic EnergyQ61459458
Radiated Energy from the 16 October 1999 Hector Mine Earthquake: Regional and Teleseismic EstimatesQ97063088
Apparent break in earthquake scaling due to path and site effects on deep borehole recordingsQ97621608
Stress drops and radiated energies of aftershocks of the 1994 Northridge, California, earthquakeQ97866247
Static and Dynamic Scaling Relations for Earthquakes and Their Implications for Rupture Speed and Stress DropQ98753031
Reconciling Teleseismic and Regional Estimates of Seismic EnergyQ98753413
Stable and Transportable Regional Magnitudes Based on Coda-Derived Moment-Rate SpectraQ98753782
Seismicity in Deep Gold Mines of South Africa: Implications for Tectonic EarthquakesQ98754039
Moment, energy, stress drop, and source spectra of western United States earthquakes from regional coda envelopesQ98807155
Coda-derived source spectra, moment magnitudes and energy-moment scaling in the western AlpsQ98969136
P433issue10
P577publication date2005-01-01
P1433published inGeophysical Research LettersQ5535576
P1476titleEvidence for non-constant energy/moment scaling from coda-derived source spectra
P478volume32

Reverse relations

cites work (P2860)
Q989691352-D or not 2-D, that is the question: A northern California test
Q98969132A new spectral ratio method using narrow band coda envelopes: Evidence for non-self-similarity in the Hector Mine sequence
Q98959566Are the Stress Drops of Small Earthquakes Good Predictors of the Stress Drops of Moderate‐to‐Large Earthquakes?
Q104176480Comparison of direct and coda wave stress drop measurements for the Wells, Nevada, earthquake sequence
Q59837684Earthquake scaling characteristics and the scale-(in)dependence of seismic energy-to-moment ratio: Insights from KiK-net data in Japan
Q60704398Measurements of spectral similarity for microearthquakes in western Nagano, Japan
Q66720694Radiated seismic energy from coda measurements and no scaling in apparent stress with seismic moment
Q98969133Regional body-wave attenuation using a coda source normalization method: Application to MEDNET records of earthquakes in Italy
Q104176460Source Complexity of the 2015 Mw 4.0 Guthrie, Oklahoma Earthquake
Q60704400Source scaling relationships of microearthquakes at Parkfield, CA, determined using the SAFOD Pilot Hole Seismic Array
Q59846512Spatial and Temporal Variations in Earthquake Stress Drop on Gofar Transform Fault, East Pacific Rise: Implications for Fault Strength
Q59848974Stress drops and radiated seismic energies of microearthquakes in a South African gold mine
Q98969134The scaling of seismic energy with moment: Simple models compared with observations

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