Magmatic Systems
Michael P. Ryan · James R. Holton · Renata Dmowska
ágú. 1994 · International Geophysics Bók 57 · Academic Press
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401
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reportEinkunnir og umsagnir eru ekki staðfestar Nánar
Um þessa rafbók
With its integrated and cohesive coverage of the current research, Magmatic Systems skillfully explores the physical processes, mechanics, and dynamics of volcanism. The text utilizes a synthesized perspective--theoretical, experimental, and observational--to address the powerful regulatory mechanisms controlling the movement of melts and cooling, with emphasis on mantle plumes, mid-ocean ridges, and intraplate magmatism. Further coverage of subduction zone magmatism includes:Fluid mechanics of mixed magma migrationInternal structure of active systemsGrain-scale melt flowRheology of partial meltsNumerical simulation of porous media melt migrationNonlinear (chaotic and fractal) processes in magma transportIn all, Magmatic Systems will prove invaluable reading to those in search of an interdisciplinary perspective on this active topic.Key Features* Fluid mechanics of magma migration from surface region to eruption site* Internal structure of active magmatic systems* Grain-scale melt flow in mantle plumes and beneath mid-ocean ridges* Physics of magmatic systems and magma dynamics
Um höfundinn
James R. Holton was Professor of Atmospheric Sciences at the University of Washington until his death in 2004. A member of the National Academies of Science, during his career he was awarded every major honor available in the atmospheric sciences including AGU’s Revelle Medal.
Renata Dmowska works in the School of Engineering and Applied Sciences at Harvard University in Cambridge, MA, USA.
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