During September 1975, three creepmeters were installed across the Imperial fault and one across the southern end of the Brawley fault, two members of the San Andreas fault system in the Imperial Valley of southeastern California. These supplement earlier installations in the Imperial Valley of one dial-gauge creepmeter and six alignment arrays (Figure 1 and Table 1). Each creepmeter uses either an invar or a stainless steel wire suspended in a horizontally buried pipe, and crosses the fault at an angle of about 45°. Those at Heber Road and Tuttle Ranch are of the design described by Yamashita and Burford (1973), using a linear variable differential transformer as the displacement transducer, and are 20 m long. The three more north...
Immediately following the 1966 Parkfield earthquake a continuing program of fault displacement measu...
The Borrego Mountain earthquake of April 9, 1968, triggered small but consistent surface displaceme...
Comparison in 1931 of the findings of field investigation in 1930 of the earthquakes of February 25 ...
During September 1975, three creepmeters were installed across the Imperial fault and one across th...
Following the 1966 Parkfield‐Cholame (California) earthquakes a creepmeter was installed across the ...
Taken together, 12 years of alinement-array data, 4 years of creepmeter records from four instrumen...
Measurements of slip on major faults in southern California have been performed over the past 18 yr ...
Four invar-wire strainmeters have been operated in shallow trench sites for 19 months beside the San...
Alignment arrays and creepmeters spanning several faults in southern California recorded slip associ...
The Global Positioning System (GPS) data collected in southern California from 1986 to 1989 indicate...
and from other creepmeters on the San Andreas fault in central California and from the Coachella Val...
This dissertation focuses on observations and modeling of fault creep in California aiming to unders...
The Brawley fault zone (bfz) and the Brawley Seismic Zone constitute the principal transfer zone acc...
Five out of six functioning creepmeters on southern California faults recorded slip triggered at the...
Surficial slip along the entire mapped length of the Superstition Hills fault in southern California...
Immediately following the 1966 Parkfield earthquake a continuing program of fault displacement measu...
The Borrego Mountain earthquake of April 9, 1968, triggered small but consistent surface displaceme...
Comparison in 1931 of the findings of field investigation in 1930 of the earthquakes of February 25 ...
During September 1975, three creepmeters were installed across the Imperial fault and one across th...
Following the 1966 Parkfield‐Cholame (California) earthquakes a creepmeter was installed across the ...
Taken together, 12 years of alinement-array data, 4 years of creepmeter records from four instrumen...
Measurements of slip on major faults in southern California have been performed over the past 18 yr ...
Four invar-wire strainmeters have been operated in shallow trench sites for 19 months beside the San...
Alignment arrays and creepmeters spanning several faults in southern California recorded slip associ...
The Global Positioning System (GPS) data collected in southern California from 1986 to 1989 indicate...
and from other creepmeters on the San Andreas fault in central California and from the Coachella Val...
This dissertation focuses on observations and modeling of fault creep in California aiming to unders...
The Brawley fault zone (bfz) and the Brawley Seismic Zone constitute the principal transfer zone acc...
Five out of six functioning creepmeters on southern California faults recorded slip triggered at the...
Surficial slip along the entire mapped length of the Superstition Hills fault in southern California...
Immediately following the 1966 Parkfield earthquake a continuing program of fault displacement measu...
The Borrego Mountain earthquake of April 9, 1968, triggered small but consistent surface displaceme...
Comparison in 1931 of the findings of field investigation in 1930 of the earthquakes of February 25 ...