Publications
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Implications of the earthquake cycle for inferring fault locking on the Cascadia megathrust Implications of the earthquake cycle for inferring fault locking on the Cascadia megathrust
GPS velocity fields in the Western US have been interpreted with various physical models of the lithosphere-asthenosphere system: (1) time-independent block models; (2) time-dependent viscoelastic-cycle models, where deformation is driven by viscoelastic relaxation of the lower crust and upper mantle from past faulting events; (3) viscoelastic block models, a time-dependent variation of...
Authors
Frederick Pollitz, Eileen Evans
Evaluation of performance of Taiwan housing stock and schools during the Mw6.4 Kaohsiung/Meinong Earthquake of February 6, 2016 Evaluation of performance of Taiwan housing stock and schools during the Mw6.4 Kaohsiung/Meinong Earthquake of February 6, 2016
The recent Kaohsiung Meinong Earthquake which occurred on February 6, 2016 affected several categories of building stock for which risk identification programs were previously developed by NCREE. A typical building type in the city of Tainan is a mixed-use three-to-five-story structure. The ground floor of this typical structure is an open-front commercial or manufacturing space, which...
Authors
Ramon Gilsanz, Cathy Huang, Jessica Mandrick, Joe Mugford, Shyh-Jiann Hwang, Tsung-Chih Chiou, Mehmet Celebi
Buildings (EERI Earthquake Reconnaissance Team Report: M7.8 Gorkha, Nepal Earthquake on April 25, 2015 and its Aftershocks) Buildings (EERI Earthquake Reconnaissance Team Report: M7.8 Gorkha, Nepal Earthquake on April 25, 2015 and its Aftershocks)
The most common building typologies in Nepal are reinforced concrete (RC) frame buildings with masonry infill walls, unreinforced masonry (URM) bearing wall buildings, and wood frame buildings (Figure 5-1). The RC frames with masonry infills are commonly constructed in urban and semi-urban areas. Most of these buildings are three to five stories high, and most privately owned buildings...
Authors
Hemant Kaushik, John Bevington, Kishor S. Jaiswal, Bret Lizundia, Surya Shrestha
Seismic‐hazard forecast for 2016 including induced and natural earthquakes in the central and eastern United States Seismic‐hazard forecast for 2016 including induced and natural earthquakes in the central and eastern United States
The U.S. Geological Survey (USGS) has produced a one‐year (2016) probabilistic seismic‐hazard assessment for the central and eastern United States (CEUS) that includes contributions from both induced and natural earthquakes that are constructed with probabilistic methods using alternative data and inputs. This hazard assessment builds on our 2016 final model (Petersen et al., 2016) by...
Authors
Mark D. Petersen, Charles Mueller, Morgan P. Moschetti, Susan M. Hoover, Andrea L. Llenos, William L. Ellsworth, Andrew J. Michael, Justin L. Rubinstein, Arthur F. McGarr, Kenneth S. Rukstales
Building damage survey and microtremor measurements for the source region of the 2015 Gorkha, Nepal, earthquake Building damage survey and microtremor measurements for the source region of the 2015 Gorkha, Nepal, earthquake
We performed a damage survey of buildings and carried out microtremor observations in the source region of the 2015 Gorkha earthquake. Our survey area spans the Kathmandu valley and areas to the east and north of the valley. Damage of buildings in the Kathmandu valley was localized, and the percentage of the totally collapsed buildings was less than 5 %. East of the Kathmandu valley...
Authors
Masumi Yamada, Takumi Hayashida, James Mori, Walter Mooney
Using structural damage statistics to derive macroseismic intensity within the Kathmandu valley for the 2015 M7.8 Gorkha, Nepal earthquake Using structural damage statistics to derive macroseismic intensity within the Kathmandu valley for the 2015 M7.8 Gorkha, Nepal earthquake
We make and analyze structural damage observations from within the Kathmandu valley following the 2015 M7.8 Gorkha, Nepal earthquake to derive macroseismic intensities at several locations including some located near ground motion recording sites. The macroseismic intensity estimates supplement the limited strong ground motion data in order to characterize the damage statistics. This...
Authors
Sean McGowan, Kishor S. Jaiswal, David J. Wald
2016 Eastern Section SSA Annual Meeting Report 2016 Eastern Section SSA Annual Meeting Report
Report on the Eastern Section Seismological Society of America Meeting.
Authors
Thomas L. Pratt, Christine A. Goulet, Oliver S. Boyd
Statistical tests of simple earthquake cycle models Statistical tests of simple earthquake cycle models
A central goal of observing and modeling the earthquake cycle is to forecast when a particular fault may generate an earthquake: a fault late in its earthquake cycle may be more likely to generate an earthquake than a fault early in its earthquake cycle. Models that can explain geodetic observations throughout the entire earthquake cycle may be required to gain a more complete...
Authors
Phoebe M. R. Devries, Eileen Evans
A possible source mechanism of the 1946 Unimak Alaska far-field tsunami, uplift of the mid-slope terrace above a splay fault zone A possible source mechanism of the 1946 Unimak Alaska far-field tsunami, uplift of the mid-slope terrace above a splay fault zone
In 1946, megathrust seismicity along the Unimak segment of the Alaska subduction zone generated the largest ever recorded Alaska/Aleutian tsunami. The tsunami severely damaged Pacific islands and coastal areas from Alaska to Antarctica. It is the charter member of “tsunami” earthquakes that produce outsized far-field tsunamis for the recorded magnitude. Its source mechanisms were...
Authors
Roland E. von Huene, John J. Miller, Dirk Klaeschen, Peter Dartnell
Earthquake source properties from pseudotachylite Earthquake source properties from pseudotachylite
The motions radiated from an earthquake contain information that can be interpreted as displacements within the source and therefore related to stress drop. Except in a few notable cases, the source displacements can neither be easily related to the absolute stress level or fault strength, nor attributed to a particular physical mechanism. In contrast paleo-earthquakes recorded by...
Authors
Nicholas M. Beeler, Giulio Di Toro, Stefan Nielsen
Testing geomorphology-derived rupture histories against the paleoseismic record of the southern San Andreas fault Testing geomorphology-derived rupture histories against the paleoseismic record of the southern San Andreas fault
Evidence for the 340-km-long Fort Tejon earthquake of 1857 is found at each of the high-resolution paleoseismic sites on the southern San Andreas Fault. Using trenching data from these sites, we find that the assemblage of dated paleoearthquakes recurs quasi-periodically (coefficient of variation, COV, of 0.6, Biasi, 2013) and requires ~80% of ruptures were shorter than the 1857 rupture...
Authors
Katherine M. Scharer, Ray J. Weldon, Sean Bemis
Late Quaternary offset of alluvial fan surfaces along the Central Sierra Madre Fault, southern California Late Quaternary offset of alluvial fan surfaces along the Central Sierra Madre Fault, southern California
The Sierra Madre Fault is a reverse fault system along the southern flank of the San Gabriel Mountains near Los Angeles, California. This study focuses on the Central Sierra Madre Fault (CSMF) in an effort to provide numeric dating on surfaces with ages previously estimated from soil development alone. We have refined previous geomorphic mapping conducted in the western portion of the...
Authors
Reed J. Burgette, Austin Hanson, Katherine M. Scharer, Nikolas Midttun