Laserfiche WebLink
603284-001 <br />The frequencies of exceedance of different values of peak ground and spectral <br />accelerations at the site were calculated by combining the following probability <br />functions: <br />The annual frequency of earthquakes of various magnitudes on a fault obtained from <br />the fault recurrence relationships; <br />. Given an earthquake of a certain magnitude on a certain fault, the probability <br />distribution of the location of the earthquake on the fault was obtained using the <br />selected rupture area versus magnitude relationship and assuming equal likelihood <br />of rupture along the length and some prescribed probabilities along the depth of the <br />fault; and <br />. Given an earthquake of a certain magnitude occurring at a certain distance from the <br />site, the probability distribution of ground motion at the site was obtained from the <br />selected attenuation relationships. <br />The above process is repeated a sufficient number of times to cover all the sources, <br />then summed to obtain the total seismic hazard at the site. This process results in a <br />relationship between ground motion level and the probability of being exceeded. <br />The computer program EZ-FRISK Version 7.60 Build 001 (Risk Engineering, Inc., 2011) <br />for probabilistic seismic hazard analysis was utilized to perform the PSHA. <br />Deterministic Seismic Hazard Analvsis (DSHA) <br />The DSHA consists of a four-step process (Reiter, 1990): <br />. Defining the location, geometry, and characteristics of earthquake sources relative to <br />the site; <br />. Determination of the site-to-source distance for each earthquake source defined <br />relative to the site; <br />Selection of the controlling earthquake relative to the site as defined by some ground <br />motion parameter. The controlling earthquake is defined by the seismic scenario <br />based on the above two steps that produces the largest magnitude of the ground <br />motion parameter being used; and <br />. Using the controlling earthquake, the ground motion at the site is obtained from the <br />selected attenuation relationships. <br />D-3