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Decoding Seismic Hazard Enigmas via Next-Generation Paleoseismic Analyses: With Application to the Cascadia Subduction Zone and Beyond- [electronic resource]
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Decoding Seismic Hazard Enigmas via Next-Generation Paleoseismic Analyses: With Application to the Cascadia Subduction Zone and Beyond- [electronic resource]
자료유형  
 학위논문
Control Number  
0016933893
International Standard Book Number  
9798379912956
Dewey Decimal Classification Number  
624
Main Entry-Personal Name  
Rasanen, Ryan A.
Publication, Distribution, etc. (Imprint  
[S.l.] : University of Washington., 2023
Publication, Distribution, etc. (Imprint  
Ann Arbor : ProQuest Dissertations & Theses, 2023
Physical Description  
1 online resource(323 p.)
General Note  
Source: Dissertations Abstracts International, Volume: 85-01, Section: B.
General Note  
Advisor: Maurer, Brett.
Dissertation Note  
Thesis (Ph.D.)--University of Washington, 2023.
Restrictions on Access Note  
This item must not be sold to any third party vendors.
Summary, Etc.  
요약In regions of infrequent moderate-to-large earthquakes, historic earthquake catalogs are often insufficient to provide inputs to seismic-hazard analyses (i.e., fault locations and magnitude-frequency relations) or to inform ground-motion predictions for certain seismic sources. As a result, analyses of macroseismic evidence (e.g., landslides, liquefaction, and felt intensities) are commonly used to help elucidate the seismic record, thereby reducing seismic-hazard uncertainty. However, while paleoseismic studies have been performed widely, existing inverse-analysis techniques (i.e., to constrain the causative earthquake magnitude and/or ground motions) have several shortcomings. Foremost, they are generally deterministic and require that the location of fault rupture be known, when in reality there are numerous uncertainties, and the source location is typically unknown. Accordingly, this dissertation (1) proposes a novel, flexible inversion methodology for analyzing paleoseismic evidence, resulting in probabilistic constraint of the seismic-source parameters (e.g., rupture location and magnitude), to the degree that the observational evidence permits. Following from (1), the methodology is tested using simulated paleoseismic studies of modern (2) liquefaction and (3) landslides. Following these simulated studies, from which lessons for forward use are gleaned, the methodology is (4) applied to evidence produced by the 1886 Charleston, SC earthquake, thereby constraining its seismic source in a more complete and transparent manner than previously available. Next, paleoliquefaction evidence in the U.S. Pacific Northwest (PNW) is (5) compiled into a community database and liquefaction in an Mw9 Cascadia Subduction Zone (CSZ) event is forecasted regionally using 30 different physics-based ground motion realizations and a first-order geospatial liquefaction model. These products are (6) made available as an online database so that others may study, and benefit from, the compiled data. Lastly, liquefaction resulting from Mw9 CSZ earthquakes is predicted at select locations using subsurface test data and more advanced geotechnical methods. As a precursor, (7) liquefaction models based on the cone penetration test (CPT) are tested in the PNW via compilation and analysis of case histories from the 2001 Nisqually, WA, earthquake. Following model testing, (8) Mw9 liquefaction is predicted for each of the 30 ground-motion simulations at 400 locations where CPT data is available. These predictions suggest that liquefaction could be both pervasive in the region and affect numerous significant hubs of population, transportation, and commerce. These predictions are compared to the evidence from (5) to assess which of the 30 simulations represent more and less plausible realizations of the motions experienced in 1700. This comparison suggests that all simulations predict far more liquefaction than has been found and that shaking intensities in 1700 may have been less in inland hubs (e.g., Seattle, Portland, and Vancouver), than prevailing forecasts indicate. The uncertainties associated with this possibility are discussed in detail.
Subject Added Entry-Topical Term  
Civil engineering.
Subject Added Entry-Topical Term  
Geophysics.
Index Term-Uncontrolled  
Cascadia Subduction Zone
Index Term-Uncontrolled  
Earthquake
Index Term-Uncontrolled  
Liquefaction
Index Term-Uncontrolled  
Nisqually earthquake
Index Term-Uncontrolled  
Paleoseismology
Index Term-Uncontrolled  
Seismic Hazard
Added Entry-Corporate Name  
University of Washington Civil and Environmental Engineering
Host Item Entry  
Dissertations Abstracts International. 85-01B.
Host Item Entry  
Dissertation Abstract International
Electronic Location and Access  
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Control Number  
joongbu:639135
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