Titlebook: Deformation and Gravity Change: Indicators of Isostasy, Tectonics, Volcanism, and Climate Change; Detlef Wolf,José Fernández Conference pr

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Propagator-matrix Technique for the Viscoelastic Response of a Multi-layered Sphere to Surface Toroal numerical methods for 2-D and 3-D glacial-isostatic adjustment (GIA) modelling have been applied recently. The present analytical approach may be used as an aid for testing more general algorithms of GIA. The propagator-matrix solution has been tested by comparing it with the analytical solution

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Shear-wave Velocity Structure around Teide Volcano: Results Using Microtremors with the SPAC Methode present an analysis of microtremor measurements recorded during the performance tests of two temporary seismic arrays installed in the eastern portion of the Teide caldera in 1994. We take advantage of recent developments of the SPAC method and use spatial cross-correlation computations to estimat

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Steric Sea-level Variations Inferred from Combined Topex/Poseidon Altimetry and GRACE Gravimetry,an sea level (GMSL) based on Topex/Poseidon (T/P) altimetry with time-variable geoid averaged over the oceans, as observed by the GRACE (Gravity Recovery and Climate Experiment) satellite. In effect, altimetry-derived GMSL changes results from two contributions: Steric (thermal plus salinity) effect

Hemiparesis

,Interpretation of 1992–1994 Gravity Changes around Mayon Volcano, Philippines, Using Point Sources,se of mass and pressure changes at several point sources modelled using a fast inversion process. This inversion approach attempts to fit gravity and elevation changes by combining a random search for the positions of the sources and a linear least-squares fit for the incremental mass, pressure and

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,Glacial-isostatic Adjustment and the Viscosity Structure Underlying the Vatnajökull Ice Cap, Icelanure. Iceland offers a unique case study for GIA research, with a thinner elastic lithosphere underlain by a low-viscosity zone or asthenosphere, as opposed to regions such as Fennoscandia or North America described by a thicker lithosphere, while not necessarily featuring an asthenosphere..A lateral

Acclaim

Review of Microgravity Observations at Mt. Etna: A Powerful Tool to Monitor and Study Active Volcann addition to describing the methodology for acquiring and reducing gravity data from Mt. Etna, this paper provides a collection of case studies aimed at demonstrating the potential of microgravity to investigate the plumbing system of an active volcano and detect forerunners to paroxysmal volcanic

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