2008 - Fellow of American Geophysical Union (AGU)
Her primary areas of investigation include Seismology, Aftershock, Fault, Magnitude and Foreshock. Her Seismology study frequently draws connections between adjacent fields such as Alluvium. Her study in Alluvium is interdisciplinary in nature, drawing from both Bedrock and Boundary layer.
The Aftershock study combines topics in areas such as Static stress, Microseism, Seismic wave and Sequence. Her Fault study integrates concerns from other disciplines, such as Mercalli intensity scale, Intraplate earthquake, Geothermal gradient and Induced seismicity. Her Foreshock research is multidisciplinary, incorporating perspectives in Slip, Hypocenter and Scaling.
Susan E. Hough mainly investigates Seismology, Aftershock, Magnitude, Fault and Sequence. Foreshock, Intraplate earthquake, Seismic hazard, Tectonics and Mercalli intensity scale are among the areas of Seismology where she concentrates her study. Her biological study deals with issues like Seismic zone, which deal with fields such as Crust.
Her research integrates issues of Seismic wave, Geodesy, Peak ground acceleration, Remotely triggered earthquakes and Induced seismicity in her study of Aftershock. Her studies deal with areas such as Geological survey, Epicenter and Range as well as Magnitude. Specifically, her work in Fault is concerned with the study of Surface rupture.
Her scientific interests lie mostly in Seismology, Foreshock, Near and far field, Fault and Aftershock. Her Seismology research is multidisciplinary, relying on both Magnitude and Sequence. Her Foreshock research is multidisciplinary, incorporating elements of Geodynamics, Induced seismicity, Earthquake swarm and Fault trace.
Her work on Seismic gap as part of general Fault study is frequently linked to Oil field, bridging the gap between disciplines. The various areas that she examines in her Aftershock study include Hypocenter, Subduction, Intraplate earthquake and Moment magnitude scale. Her study in Seismic hazard is interdisciplinary in nature, drawing from both Range and Sediment.
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A MODEL FOR THE SHAPE OF THE FOURIER AMPLITUDE SPECTRUM OF ACCELERATION AT HIGH FREQUENCIES
John G. Anderson;Susan E. Hough.
Bulletin of the Seismological Society of America (1984)
Near-Field Investigations of the Landers Earthquake Sequence, April to July 1992
Kerry Sieh;Lucile M Jones;Egill Hauksson;Kenneth W Hudnut.
Science (1993)
Remotely Triggered Seismicity on the United States West Coast following the Mw 7.9 Denali Fault Earthquake
S. G. Prejean;D. P. Hill;E. E. Brodsky;S. E. Hough.
Bulletin of the Seismological Society of America (2004)
On the Modified Mercalli intensities and magnitudes of the 1811–1812 New Madrid earthquakes
Susan E. Hough;John G. Armbruster;Leonardo Seeber;Jerry F. Hough.
Journal of Geophysical Research (2000)
Intensity, magnitude, location and attenuation in India for felt earthquakes since 1762
Walter Szeliga;Susan E Hough;Stacey S Martin;Roger D Bilham.
Bulletin of the Seismological Society of America (2010)
High-frequency spectra observed at Anza, California: Implications for Q structure
S. E. Hough;J. G. Anderson.
Bulletin of the Seismological Society of America (1988)
Attenuation near Anza, California
S. E. Hough;J. G. Anderson;J. Brune;F. Vernon.
Bulletin of the Seismological Society of America (1988)
Observations of Loma Prieta aftershocks from a dense array in Sunnyvale, California
Arthur Frankel;Susan Hough;Paul Friberg;Robert Busby.
Bulletin of the Seismological Society of America (1991)
Localized damage caused by topographic amplification during the 2010 M 7.0 Haiti earthquake
Susan E. Hough;Jean Robert Altidor;Dieuseul Anglade;Doug Given.
Nature Geoscience (2010)
Using microtremors to assess potential earthquake site response: A case study in Flushing Meadows, New York City
E. H. Field;S. E. Hough;K. H. Jacob.
Bulletin of the Seismological Society of America (1990)
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