Radar interferometry and its application to changes in the Earth's surface
D Massonnet, KL Feigl - Reviews of geophysics, 1998 - Wiley Online Library
Geophysical applications of radar interferometry to measure changes in the Earth's surface
have exploded in the early 1990s. This new geodetic technique calculates the interference …
have exploded in the early 1990s. This new geodetic technique calculates the interference …
Magma chambers: Formation, local stresses, excess pressures, and compartments
A Gudmundsson - Journal of Volcanology and Geothermal Research, 2012 - Elsevier
An existing magma chamber is normally a necessary condition for the generation of a large
volcanic edifice. Most magma chambers form through repeated magma injections …
volcanic edifice. Most magma chambers form through repeated magma injections …
Drainage of a deep magma reservoir near Mayotte inferred from seismicity and deformation
The dynamics of magma deep in the Earth's crust are difficult to capture by geophysical
monitoring. Since May 2018, a seismically quiet area offshore of Mayotte in the western …
monitoring. Since May 2018, a seismically quiet area offshore of Mayotte in the western …
[LIBRO][B] Physics of the Earth
FD Stacey, PM Davis - 2008 - books.google.com
The fourth edition of Physics of the Earth maintains the original philosophy of this classic
graduate textbook on fundamental solid earth geophysics, while being completely revised …
graduate textbook on fundamental solid earth geophysics, while being completely revised …
Deformation from inflation of a dip** finite prolate spheroid in an elastic half‐space as a model for volcanic stressing
XM Yang, PM Davis, JH Dieterich - Journal of Geophysical …, 1988 - Wiley Online Library
Exact analytic expressions are given for the deformation field resulting from inflation of a
finite prolate spheroidal cavity in an infinite elastic medium. The field is equivalent to that …
finite prolate spheroidal cavity in an infinite elastic medium. The field is equivalent to that …
Elastic stress and deformation near a finite spherical magma body: Resolution of the point source paradox
DF McTigue - Journal of Geophysical Research: Solid Earth, 1987 - Wiley Online Library
Approximate solutions are obtained for the stress and displacement fields due to a
pressurized spherical cavity in an elastic half‐space. The solutions take the form of series …
pressurized spherical cavity in an elastic half‐space. The solutions take the form of series …
Sensitivity analysis for volcanic source modeling quality assessment and model selection
F Cannavó - Computers & geosciences, 2012 - Elsevier
The increasing knowledge and understanding of volcanic sources has led to the
development and implementation of sophisticated and complex mathematical models with …
development and implementation of sophisticated and complex mathematical models with …
How local stresses control magma-chamber ruptures, dyke injections, and eruptions in composite volcanoes
A Gudmundsson - Earth-science reviews, 2006 - Elsevier
To assess the probability of a volcanic eruption during an unrest period, we must understand
magma-chamber rupture and dyke propagation to the surface, as well as dyke arrest at …
magma-chamber rupture and dyke propagation to the surface, as well as dyke arrest at …
Deformation due to a pressurized horizontal circular crack in an elastic half-space, with applications to volcano geodesy
We consider deformation due to sill-like magma intrusions using a model of a horizontal
circular crack in a semi-infinite elastic solid. We present exact expressions for vertical and …
circular crack in a semi-infinite elastic solid. We present exact expressions for vertical and …
Towards more realistic values of elastic moduli for volcano modelling
The accuracy of elastic analytical solutions and numerical models, widely used in
volcanology to interpret surface ground deformation, depends heavily on the Young's …
volcanology to interpret surface ground deformation, depends heavily on the Young's …