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Mark Simons

Researcher at California Institute of Technology

Publications -  186
Citations -  13882

Mark Simons is an academic researcher from California Institute of Technology. The author has contributed to research in topics: Interferometric synthetic aperture radar & Slip (materials science). The author has an hindex of 63, co-authored 176 publications receiving 11943 citations. Previous affiliations of Mark Simons include Massachusetts Institute of Technology.

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Coseismic Deformation from the 1999 Mw 7.1 Hector Mine, California, Earthquake as Inferred from InSAR and GPS Observations

TL;DR: In this paper, the authors use interferometric synthetic aperture radar (InSAR) and Global Positioning System (GPS) observations to investigate static deformation due to the 1999 M_w 7.1 Hector Mine earthquake, that occurred in the eastern California shear zone.
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Some thoughts on the use of InSAR data to constrain models of surface deformation : noise structure and data downsampling

TL;DR: In this paper, the authors estimate the actual covariance structure of noise in InSAR data and combine the data-covariance information with the inherent resolution of an assumed source model to develop an efficient algorithm for spatially variable data resampling.
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Deformation due to a pressurized horizontal circular crack in an elastic half-space, with applications to volcano geodesy

TL;DR: In this article, a model of a horizontal circular crack in a semi-infinite elastic solid was proposed and exact expressions for vertical and horizontal displacements of the free surface of a half-space were derived for a special case of a uniformly pressurized crack.
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A satellite geodetic survey of large-scale deformation of volcanic centres in the central Andes

TL;DR: A satellite-based interferometric synthetic aperture radar survey of the remote central Andes volcanic arc reveals the background level of activity of about 900 volcanoes, 50 of which have been classified as potentially active, and finds four centres of broad, roughly axisymmetric surface deformation.