On the Dynamics of Rhyolite Dome Emplacement: Densities and Deformation Fields

Silicic rocks in Iceland are generally associated with central volcanoes and are often emplaced on or around caldera rims. Rhyolite magma can rise, due to buoyancy forces and either form a cryptodome in the shallow crust or rise to the surface, where it erupts. Due to its high viscosity and resistan...

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Bibliographic Details
Main Author: Þorbjorg Ágústsdóttir 1981-
Other Authors: Háskóli Íslands
Format: Thesis
Language:English
Published: 2009
Subjects:
Online Access:http://hdl.handle.net/1946/16072