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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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An aseismic slip pulse in northern Chile and along‐strike variations in seismogenic behavior

TL;DR: In this article, the authors used interferometric synthetic aperture radar, GPS, and seismic observations spanning 5 to 18 years to reveal a detailed kinematic picture of the spatiotemporal evolution of fault slip in a region corresponding to the 30 July 1995 M_w 8.1 subduction zone megathrust earthquake in northern Chile.
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Accounting for prediction uncertainty when inferring subsurface fault slip

TL;DR: In this article, a new generation of earthquake source models is proposed based on a general formalism that rigorously quantifies and incorporates the impact of uncertainties in fault slip inverse problems.
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Co-seismic slip from the 1995 July 30 Mw= 8.1 Antofagasta, Chile, earthquake as constrained by InSAR and GPS observations

TL;DR: In this paper, radar interferometric and GPS observations of the displacement field from the 1995 July 30 Mw = 8.1 Antofagasta, Chile, earthquake and invert for the distribution of slip along the co-seismic fault plane were compared.
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Localization of the gravity field and the signature of glacial rebound

TL;DR: The negative free-air gravity anomaly centred on Hudson Bay, Canada, shows a remarkable correlation with the location of the Laurentide ice sheet, suggesting that this gravity anomaly is the result of incomplete post-glacial rebound as mentioned in this paper.
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Aseismic slip and seismogenic coupling along the central San Andreas Fault

TL;DR: In this paper, the authors used high-resolution Synthetic aperture radar and GPS-derived observations of surface displacements to derive the first probabilistic estimates of fault coupling along the creeping section of the San Andreas Fault, in between the terminations of the 1857 and 1906 magnitude 7.9 earthquakes.