An array of moveable seismographic trailers was deployed at three sites along the northern section of the “Big Bend” in the San Andreas fault in southern California. The three sites monitored were the Carrizo Plains, Frazier Park, and Lake Hughes areas. Effective observation times at each site ranged from 38 to 69 days. The microearthquake activity rates observed were 0.3 events/day, 3.0 events/day, and 1.9 events/day, respectively, based on the number of located events plus the number of unlocated events with S-P ≦ 3.0 sec. The majority of the activity does not appear to be directly associated with the San Andreas fault. A comparison of the activity rates observed in this study with the results of a survey conducted in the same areas by Br...
This is the published version. Copyright 1976 American Geophysical Union. All Rights Reserved.Sixtee...
Intensities of shaking for previously untapped, historical sources of damage data from the 1906 eart...
Evidence for regional seismicity is of four kinds: (1) geological field observation of fault phenome...
An array of moveable seismographic trailers was deployed at three sites along the northern section o...
An array of moveable seismographic trailers was deployed at three sites along the northern section o...
An array of moveable seismographic trailers was deployed at three sites along the northern section o...
The major, historically active San Jacinto and San Andreas fault systems pass through the San Bernar...
Microearthquakes have been systematically recorded with magnitudes down to -1.5 at 38 locations alo...
The major, historically active San Jacinto and San Andreas fault systems pass through the San Bernar...
Microearthquakes have been systematically recorded with magnitudes down to -1.5 at 38 locations alo...
The Southern California Seismic Network (SCSN) has produced the SCSN earthquake catalog from 1932 to...
The San Andreas fault is the longest fault in California and one of the longest strike-slip faults i...
We evaluate the relationships between the spatio-temporal patterns and faulting mechanisms of small ...
A unique data set of seismograms for 720 source-receiver paths has been collected as part of a cont...
This is the published version. Copyright 1976 American Geophysical Union. All Rights Reserved.Sixtee...
This is the published version. Copyright 1976 American Geophysical Union. All Rights Reserved.Sixtee...
Intensities of shaking for previously untapped, historical sources of damage data from the 1906 eart...
Evidence for regional seismicity is of four kinds: (1) geological field observation of fault phenome...
An array of moveable seismographic trailers was deployed at three sites along the northern section o...
An array of moveable seismographic trailers was deployed at three sites along the northern section o...
An array of moveable seismographic trailers was deployed at three sites along the northern section o...
The major, historically active San Jacinto and San Andreas fault systems pass through the San Bernar...
Microearthquakes have been systematically recorded with magnitudes down to -1.5 at 38 locations alo...
The major, historically active San Jacinto and San Andreas fault systems pass through the San Bernar...
Microearthquakes have been systematically recorded with magnitudes down to -1.5 at 38 locations alo...
The Southern California Seismic Network (SCSN) has produced the SCSN earthquake catalog from 1932 to...
The San Andreas fault is the longest fault in California and one of the longest strike-slip faults i...
We evaluate the relationships between the spatio-temporal patterns and faulting mechanisms of small ...
A unique data set of seismograms for 720 source-receiver paths has been collected as part of a cont...
This is the published version. Copyright 1976 American Geophysical Union. All Rights Reserved.Sixtee...
This is the published version. Copyright 1976 American Geophysical Union. All Rights Reserved.Sixtee...
Intensities of shaking for previously untapped, historical sources of damage data from the 1906 eart...
Evidence for regional seismicity is of four kinds: (1) geological field observation of fault phenome...