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Andrew V. Newman
Researcher at Georgia Institute of Technology
Publications - 69
Citations - 2761
Andrew V. Newman is an academic researcher from Georgia Institute of Technology. The author has contributed to research in topics: Subduction & Slip (materials science). The author has an hindex of 28, co-authored 68 publications receiving 2522 citations. Previous affiliations of Andrew V. Newman include University of California, Santa Cruz & Los Alamos National Laboratory.
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Teleseismic estimates of radiated seismic energy: The E/M 0 discriminant for tsunami earthquakes
Andrew V. Newman,Emile A. Okal +1 more
TL;DR: In this article, the authors adapt the formalism of Boatwright and Choy for the computation of radiated seismic energy from broadband records at teleseismic distances to the real-time situation when neither the depth nor the focal geometry of the source is known accurately.
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Slow deformation and lower seismic hazard at the new madrid seismic zone
TL;DR: Global Positioning System measurements across the New Madrid seismic zone (NMSZ) in the central United States show little, if any, motion, and frequency-magnitude relation for seismicity implies that the hazard posed by great earthquakes in the NMSZ appears to be overestimated.
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A four-dimensional viscoelastic deformation model for Long Valley Caldera, California, between 1995 and 2000
TL;DR: In this article, the authors investigate the effects of viscoelastic rheologies surrounding a vertically dipping prolate spheroid source during an active period of time-dependent deformation between 1995 and 2000 at Long Valley caldera.
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The 25 October 2010 Mentawai tsunami earthquake, from real-time discriminants, finite-fault rupture, and tsunami excitation
TL;DR: In this paper, the authors identify a rare slow-source tsunami earthquake based on disproportionately large tsunami waves, excessive rupture duration near 125 s, and predominantly shallow, near-trench slip determined through finite-fault modeling.
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Geodetic and Seismic Constraints on Recent Activity at Long Valley Caldera, California: Evidence for Viscoelastic Rheology
TL;DR: In this article, the authors developed a model consistent with these observations and also consistent with independent constraints on sub-surface rheology from thermal, geochemical and laboratory data, which is well fit by a model with a single pressure source at 6 km depth which experienced a pressure pulse that began in late 1996, peaked in November 1997, close to the time of major seismic moment release, and essentially ended in mid-1999.