Seismological studies at Parkfield VIII: Modeling the observed travel-time changes

Bulletin of the Seismological Society of America

Volumn 90, Issue 3, 2000, Pages 702-708

  Korneev, V A ^a   McEvilly, T V ^a   Karageorgi, E D ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BOREHOLE; EARTHQUAKE PRECURSOR; FAULT SLIP; HYDROLOGICAL RESPONSE; MONITORING SYSTEM; SAN ANDREAS FAULT; SEISMICITY; TRAVEL TIME;

CALIFORNIA; PARKFIELD; UNITED STATES;

EID: 0033838888     PISSN: 00371106     EISSN: None     Source Type: Journal    
DOI: 10.1785/0119990038     Document Type: Article

References (14)

1. Differential analysis of coda Q using similar microearthquakes in seismic gaps, part 2: Application to seismograms recorded by the Parkfield high resolution seismic network
2. The Parkfield, California, prediction experiment
3. Finite-difference simulation of P-SV-wave propagation: A displacement potential approach
4. Three-dimensional velocity structure, seismicity, and fault structure in the Parkfield region, central California
5. Seismological studies at Parkfield. II: Search for temporal variations in wave propagation using Vibroseis
6. Seismological studies at Parkfield IV: Variations in controlled-source waveform parameters and their correlation with seismic activity, 1987-1994
7. Characteristics of wave propagation in the San Andreas fault-zone at Parkfield: Observations and modeling
8. Fault-zone guided waves from explosions in the San Andreas fault at Parkfield and Cienega Valley, California
9. Seismological studies at Parkfield: I. Simultaneous inversion for velocity structure and hypocenters using B-splines parameterization
10. Fault slip rates at depth from recurrence intervals of repeating microearthquakes
11. Seismological studies at Parkfield III: Microearthquake clusters in the study of fault-zone dynamics
12. Fault-zone monitoring with repeating similar microearthquakes: A search for the Vibroseis anomaly at Parkfield
13. Central California foreshocks of the great 1857 earthquake
14. Characterization of the Parkfield transient: Evidence for aseismic stress transfer