Differential analysis of coda Q using similar microearthquakes in seismic gaps. Part 2: Application to seismograms recorded by the Parkfield High Resolution Seismic Network
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- Type
- article
- Published
- 1996-06-01
- Cited by
- 25
- References
- 51
- OpenAlex
- https://openalex.org/W1787999631
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:129541031
Keywords
Coda, Microearthquake, Seismology, Geology, Seismogram
References
- Seismological studies at Parkfield III: microearthquake clusters in the study of fault-zone dynamics : Bulletin - Seismological Society of America, 84 (2), 1994, pp 247–263
- Energy-flux model of seismic coda: Separation of scattering and intrinsic attenuation
- Fault zone structure determined through the analysis of earthquake arrival times
- Heterogeneous slip and rupture models of the San Andreas fault zone based upon three-dimensional earthquake tomography
- Seismological studies at Parkfield. I. Simultaneous inversion for velocity structure and hypocenters using cubic B-splines parameterization
- High-frequency borehole seismograms recorded in the San Jcinto Fault zone, Southern California Part 2. Attenuation and site effects
- OF THE 1979 IMPERIAL VALLEY, CALIFORNIA, EARTHQUAKE: EVIDENCE FOR FAULT HETEROGENEITY?
- Recurrence models and Parkfield, California, earthquakes
- Mechanisms of seismic attenuation in the crust: Scattering and anelasticity in New York State, South Africa, and southern California
- Stability of coda Q in the region of Parkfield, California: View from the U.S. Geological Survey Parkfield Dense Seismograph Array
- A comparison of earthquake coda waves at surface versus subsurface seismometers
- Quantitative measurements of shear wave polarizations at the Anza Seismic Network, southern California: Implications for shear wave splitting and earthquake prediction
- Variations in rupture process with recurrence interval in a repeated small earthquake
- Stress Diffusion Along the San Andreas Fault at Parkfield, California
- Origin of coda waves: Source, attenuation, and scattering effects
- Origins of Amplitude Variations In Seismic Doublets: Source Or Attenuation Process?
- Evidence for shallow and pervasive seismic anisotropy in the Wellington Region, New Zealand
- Clustering and Periodic Recurrence of Microearthquakes on the San Andreas Fault at Parkfield, California
- Three‐dimensional velocity structure, seismicity, and fault structure in the Parkfield Region, central California
- Earthquake swarm activity revealed from high-resolution relative hypocenters — clustering of microearthquakes
Cited by
- Temporal changes in attenuation associated with the 2004 M6.0 Parkfield earthquake
- Precise determination of the relative wave propagation parameters of similar events using a small-aperture seismic array
- Crustal changes at Mt. Etna volcano accompanying the 2002–2003 eruption as inferred from a repeating earthquake analysis
- Repeating volcano-tectonic earthquakes at Mt. Etna volcano (Sicily, Italy) during 1999–2009
- Temporal Changes of Shallow Seismic Velocity Around the Karadere-Düzce Branch of the North Anatolian Fault and Strong Ground Motion
- Seismic waveform attributes before and after the Loma Prieta earthquake: Scattering change near the earthquake and temporal recovery
- Hypocenter migration as an explanation for temporal changes in coda Q
- Precursory Rise of P-Wave Attenuation before the 2004 Parkfield Earthquake
- Coseismic and postseismic velocity changes measured by repeating earthquakes
- Motif Discovery on Seismic Amplitude Time Series: The Case Study of Mt Etna 2011 Eruptive Activity
- Temporal changes in coda Q −1 and b value due to the static stress change associated with the 1995 Hyogo‐ken Nanbu earthquake
- Anisotropy, repeating earthquakes, and seismicity associated with the 2008 eruption of Okmok volcano, Alaska
- Seismic coda attenuation after the Mw = 6.2 Armenia (Colombia) earthquake of 25 January 1999
- Monitoring rapid temporal change in a volcano with coda wave interferometry
- Changes in the Coda Decay Rate and Shear-Wave Splitting Parameters Associated with Seismic Swarms at Mt. Vesuvius, Italy
- Seismological Studies at Parkfield VIII: Modeling the Observed Travel-Time Changes
- Short Note Temporal Stability of Coda Q 1 in Southern California
- Seismological studies at Parkfield IV: Variations in controlled-source waveform parameters and their correlation with seismicity, 1987 to 1995
- Evidence for stability in coda Q associated with the Egion (central Greece) earthquake of 15 June 1995
- Enhanced Observations with Borehole Seismographic Networks. The Parkfield, California Experiment
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