Geologic map of the San Andreas fault zone in San Andreas Lake, San Mateo County, California

10.3133/mf652 ◽  
1975 ◽  
Keyword(s):  
Fault Zone ◽  
San Andreas Fault ◽  
San Andreas ◽  
Geologic Map ◽  
San Mateo County

scholarly journals Fine-scale delineation of the location of and relative ground shaking within the San Andreas Fault zone at San Andreas Lake, San Mateo County, California

2013 ◽  
pp. i-53 ◽  
Author(s):  
R.D. Catchings ◽  
M.J. Rymer ◽  
M.R. Goldman ◽  
C.S. Prentice ◽  
R.R. Sickler
Keyword(s):  
Fault Zone ◽  
San Andreas Fault ◽  
Fine Scale ◽  
Ground Shaking ◽  
San Andreas ◽  
San Mateo County

Preliminary report on drilling in and near the San Andreas fault zone, California; Dry Lake Valley No. 1

1979 ◽  
Author(s):  
John C. Roller ◽  
M.D. Zoback ◽  
C.B. Raleigh ◽  
R.P. Leichti
Keyword(s):  
Fault Zone ◽  
Preliminary Report ◽  
San Andreas Fault ◽  
San Andreas ◽  
Dry Lake

Water-level fluctuations and earthquakes on the San Andreas fault zone

Geology ◽  
1975 ◽  
Vol 3 (8) ◽  
pp. 437 ◽  
Author(s):  
Robert L. Kovach ◽  
Amos Nur ◽  
Robert L. Wesson ◽  
Russell Robinson
Keyword(s):  
Water Level ◽  
Fault Zone ◽  
San Andreas Fault ◽  
Water Level Fluctuations ◽  
San Andreas

Interpretation of seismic reflection profiling data for the structure of the San Andreas fault zone

1983 ◽  
Vol 73 (6A) ◽  
pp. 1701-1720
Author(s):  
R. Feng ◽  
T. V. McEvilly
Keyword(s):  
Fault Zone ◽  
Seismic Reflection ◽  
San Andreas Fault ◽  
Velocity Model ◽  
Seismic Reflection Profile ◽  
Lateral Velocity ◽  
Zone Structure ◽  
Ray Method ◽  
Velocity Change ◽  
San Andreas

Abstract A seismic reflection profile crossing the San Andreas fault zone in central California was conducted in 1978. Results are complicated by the extreme lateral heterogeneity and low velocities in the fault zone. Other evidence for severe lateral velocity change across the fault zone lies in hypocenter bias and nodal plane distortion for earthquakes on the fault. Conventional interpretation and processing methods for reflection data are hard-pressed in this situation. Using the inverse ray method of May and Covey (1981), with an initial model derived from a variety of data and the impedance contrasts inferred from the preserved amplitude stacked section, an iterative inversion process yields a velocity model which, while clearly nonunique, is consistent with the various lines of evidence on the fault zone structure.

(U–Th)/He thermochronometry reveals Pleistocene punctuated deformation and synkinematic hematite mineralization in the Mecca Hills, southernmost San Andreas Fault zone

2017 ◽  
Vol 476 ◽  
pp. 87-99 ◽  
Author(s):  
Amy C. Moser ◽  
James P. Evans ◽  
Alexis K. Ault ◽  
Susanne U. Janecke ◽  
Kelly K. Bradbury
Keyword(s):  
Fault Zone ◽  
San Andreas Fault ◽  
San Andreas
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