Journal ArticleDOI
A four-dimensional viscoelastic deformation model for Long Valley Caldera, California, between 1995 and 2000
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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.About:
This article is published in Journal of Volcanology and Geothermal Research.The article was published on 2006-02-01. It has received 158 citations till now. The article focuses on the topics: Slip (materials science).read more
Citations
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Silicic magma reservoirs in the Earth's crust
Olivier Bachmann,Christian Huber +1 more
TL;DR: In this article, the authors focus on recent claims that magma columns within the Earth's crust are mostly kept at high crystallinity (mush zones) and that the dynamics within those mush columns, albeit modulated by external factors (e.g., regional stress field, rheology of the crust, pre-existing tectonic structure), play an important role in controlling how magmas evolve, degas, and ultimately erupt.
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Catastrophic caldera-forming eruptions: Thermomechanics and implications for eruption triggering and maximum caldera dimensions on Earth
TL;DR: In this paper, the authors used temperature-dependent, viscoelastic numerical models that incorporate a Mohr-Coulomb failure criterion to find that eruptive failure of the largest magma chambers is a function of the geometry of the overlying roof and the location of the brittle-ductile transition.
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Duration, magnitude, and frequency of subaerial volcano deformation events: New results from Latin America using InSAR and a global synthesis
TL;DR: In this paper, satellite-based interferometric synthetic aperture radar (InSAR) was used to make the first systematic search for deformation in all volcanic arcs of Latin America (including Mexico, Central America, the Caribbean, and the northern and southern Andes), spanning 2006-2008.
Journal ArticleDOI
Surface deformation of Long Valley caldera and Mono Basin, California, investigated with the SBAS-InSAR approach
Pietro Tizzani,Paolo Berardino,Francesco Casu,Francesco Casu,P. Euillades,P. Euillades,Mariarosaria Manzo,Mariarosaria Manzo,G. P. Ricciardi,Giovanni Zeni,Giovanni Zeni,Riccardo Lanari +11 more
TL;DR: In this paper, the surface deformation of the eastern California area that includes Long Valley caldera and Mono Basin was investigated using the Small BAseline Subset (SBAS) approach.
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Magma intrusion and deformation predictions: Sensitivities to the Mogi assumptions
TL;DR: In this article, the authors compute surface displacement due to SESs at depth using a combination of analytical and finite element models (FEMs), for which the HIPSHS assumptions are not required.
References
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Book
Numerical Recipes in FORTRAN
TL;DR: The Diskette v 2.04, 3.5'' (720k) for IBM PC, PS/2 and compatibles [DOS] Reference Record created on 2004-09-07, modified on 2016-08-08.
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New, improved version of generic mapping tools released
Paul Wessel,Walter H. F. Smith +1 more
TL;DR: GMT allows users to manipulate (x,y,z) data, and generate PostScript illustrations, including simple x-y diagrams, contour maps, color images, and artificially illuminated, perspective, and/or shaded-relief plots using a variety of map projections.
Journal ArticleDOI
REVEL: A model for Recent plate velocities from space geodesy
TL;DR: In this article, the relative velocities of 19 plates and continental blocks were derived from publicly available space geodetic (primarily GPS) data for the period 1993-2000, including an independent and rigorous estimate for GPS velocity uncertainties to assess plate rigidity and propagate these uncertainties to the velocity estimates.
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The displacement fields of inclined faults
Lalu Mansinha,D. E. Smylie +1 more
TL;DR: In this article, closed analytical expressions for the displacement fields of inclined, finite strike-slip and dip-slink faults are given, and they may be readily used in the numerical computation of displacements, and by differentiation, strain and stress fields may be derived.