Effect of host-rock rheology on dyke shape, thickness and magma overpressure
| Autor: | Christoph F. Hieronymus, Remi Vachon |
|---|---|
| Rok vydání: | 2016 |
| Předmět: |
Elasticity and anelasticity
geography and modelling geography.geographical_feature_category Plasticity Geofysik 010504 meteorology & atmospheric sciences diffusion Mechanics crust and lithosphere [Rheology] 010502 geochemistry & geophysics Numerical solutions 01 natural sciences Overpressure Geophysics Rheology Volcano Physics of magma and magma bodies Geochemistry and Petrology Magma and creep theory Petrology Geology 0105 earth and related environmental sciences |
| Zdroj: | Geophysical Journal International. 208:1414-1429 |
| ISSN: | 1365-246X 0956-540X |
| DOI: | 10.1093/gji/ggw448 |
| Popis: | The size and thickness of dykes is of fundamental importance for volcano dynamics because dykes are the primary path for magma transport, and because large numbers of dykes often comprise a major proportion of the volcanic edifice and of the underlying crust. Standard elastic models predict dyke geometry to be elliptic in cross-section for constant overpressure and uniform host-rock properties, whereas observations show that dyke thickness is typically more nearly constant with a sharp taper at the ends. Moreover, the predicted overpressures required to inflate dykes in a purely elastic medium are often significantly higher (> 150 MPa and up to 2 GPa) than those estimated by other means (about 1-50 MPa). In this study, we use 2-D finite element models to test whether other host-rock rheologies lead to more realistic dyke shapes and overpressures. We examine three different rheologies, each of which is affected by the presence of the dyke itself: (1) elasticity with reduced moduli in regions of low pressure or tension; (2) elastoplasticity with plastic failure in the high-stress regions surrounding the dyke tips; (3) viscoelasticity with a viscosity decrease due to heating by the dyke. We use rheological parameters obtained from laboratory experiments whenever possible, and assume static conditions for the final dyke shape. We find that all three rheologies tend to make the dyke more rectangular relative to the elliptical dykes of the linearly elastic models. The change in shape is due to enhanced deformation in the high-stress zone surrounding the dyke tip. We also find that the overpressure required to inflate an initially thin dyke to a given thickness is reduced for all three rheologies. The greatest decrease in overpressure by a factor of about 0.1 is observed for the elastoplastic model, and for the viscoelastic model if the dyke intrudes into moderately pre-heated host-rock. We discuss our results with respect to dyke observations from Rum Island (Scotland) and use these as a guide to evaluate our models. |
| Databáze: | OpenAIRE |
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