

Type of Document Master's Thesis Author Student, Heather H. URN etd-2143122449761431 Title Assessing the Seismic Hazard in Charleston, South Carolina: Comparisons Among Statistical Models Degree Master of Science Department Geological Sciences Advisory Committee
Advisor Name Title Martin, James R. II Robinson, Edwin S. Snoke, J. Arthur Committee Chair Keywords
- seismic hazard
- intraplate earthquakes
- strong ground motion
- paleoliquefacation
- charleston
- south carolina
Date of Defense 1997-01-27 Availability unrestricted Abstract Seismic hazard calculations for sites in eastern North
America have traditionally assumed a Poisson process to
describe the temporal behavior of earthquakes and have
employed the Gutenberg-Richter relationship to define the
frequency distribution of earthquake magnitude. For sites
in areas where geological information indicates recurrent,
large earthquakes, however, such data imply a rate for
large events which often exceeds that predicted by the
Gutenberg-Richter relationship. One way in which this
discrepancy can be reconciled is to assume that the larger
events occur as a time-dependent, or renewal, process
and possess a "characteristic earthquake" magnitude
distribution. The main purpose of this study is to make a
quantitative comparison of seismic hazard estimates for
Charleston of the influences of 1) the Poisson temporal
model assuming the Gutenberg-Richter and characteristic
earthquake magnitude recurrence relationships with 2) the
renewal temporal model assuming the characteristic
magnitude recurrence relationship. Other issues that are
examined are the sensitivity of uncertainties of hazard
model parameters such as maximum magnitude and
seismic source delineation.
Probabilistic seismic hazard calculations for the next 50
years were performed at Charleston for all potential
seismic sources. The highest estimate of seismic hazard
was obtained with the Poisson temporal model and
characteristic earthquake recurrence relationship. The
lowest hazard was obtained with the renewal temporal
model and characteristic magnitude recurrence
relationship. The results of this study are in good
agreement with hazard estimates for Charleston in the most
recent national seismic hazard maps.
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