Ground Motion Hazard and Scenario Design Earthquakes Including Source Rupture Effects, Case in Study: City of San Francisco

2009 ◽  
Vol 25 (2) ◽  
pp. 379-414 ◽  
Author(s):  
Badie Rowshandel

Using a probabilistic approach, a directivity model, and the fault and seismicity database of the California Geological Survey, one-second spectral accelerations for a site in the city of San Francisco are computed for several fault rupture types. Five rupture scenarios were investigated. Of these, two cases involve random distribution of hypocenters and two are “limiting cases,” resulting in the lower-bound and the upper-bound ground motions at the site. Deaggregation of hazard in terms of magnitude, distance, epsilon, and directivity for the rupture scenarios studied reveals that three scenario events dominate ground motion hazard at the site. Expressed in terms of modal values of the hazard parameters, these are: (1) [Formula: see text], [Formula: see text], (2) [Formula: see text], [Formula: see text], and (3) [Formula: see text], [Formula: see text]. The relative significance of these scenario events varies mostly with rupture type and to lesser degrees with site condition and return period. The first scenario event is a repeat of the 1906 San Francisco earthquake. The second represents the impact of the San Gregorio fault and North-Coast and Offshore segments of the San Andreas fault, and the third reflects the seismicity mainly on the Peninsula and the Santa Cruz Mountains segments of the San Andreas fault.

2018 ◽  
Author(s):  
Carol S. Prentice ◽  
◽  
Robert R. Sickler ◽  
Kevin B. Clahan ◽  
Alexandra Pickering ◽  
...  

1964 ◽  
Vol 54 (1) ◽  
pp. 67-77
Author(s):  
Robert M. Hamilton ◽  
Alan Ryall ◽  
Eduard Berg

abstract To determine a crustal model for the southwest side of the San Andreas fault, six large quarry blasts near Salinas, California, were recorded at 27 seismographic stations in the region around Salinas, and along a line northwest of the quarry toward San Francisco. Data from these explosions are compared with results of explosion-seismic studies carried out by the U.S. Geological Survey on a profile along the coast of California from San Francisco to Camp Roberts. The velocity of Pg, the P wave refracted through the crystalline crust, in the Salinas region is 6.2 km/sec and the velocity of Pn is about 8.0 km/sec. Velocities of the direct P wave in near-sur-face rocks vary from one place to another, and appear to correlate well with gross geologic features. The thickness of the crust in the region southwest of the San Andreas fault from Salinas to San Francisco is about 22 kilometers.


1968 ◽  
Vol 58 (6) ◽  
pp. 1955-1973
Author(s):  
Stewart W. Smith ◽  
Max Wyss

ABSTRACT Immediately following the 1966 Parkfield earthquake a continuing program of fault displacement measurements was undertaken, and several types of instruments were installed in the fault zone to monitor ground motion. In the year subsequent to the earthquake a maximum of at least 20 cm of displacement occurred on a 30 km section of the San Andreas fault, which far exceeded the surficial displacement at the time of the earthquake. The rate of displacement decreased logarithmically during this period in a manner similar to that of the decrease in aftershock activity. After the initial high rate of activity it could be seen that most of the displacement was occurring in 4–6 day epochs of rapid creep following local aftershocks. The variation of fault displacement along the surface trace was measured and shown to be consistent with a vertidal fault surface 44 km long and 14 km deep, along which a shear stress of 2.4 bars was relieved.


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