Links between magma- tectonic rate balances, plutonism, and volcanism
Journal of Geophysical Research
By: H. R. Shaw
Links
- The Publications Warehouse does not have links to digital versions of this publication at this time
- Download citation as: RIS | Dublin Core
Abstract
With Smith's (1979) model of ash flow magmatism as the point of departure, quantitative regimes of crustal magmatic evolution are outlined. The average extrusive regime of ash flow magmatism operates at a rate of about 0.001 km3/yr; progressively larger episodes of increasing repose times characterize the evolution of caldera-forming eruptions. Categorical examples of the principal types of igneous path are discussed relative to continental basalt, silicic ash flow, batholithic granite, and intrusive porphyry systems.-from Author
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Links between magma- tectonic rate balances, plutonism, and volcanism |
| Series title | Journal of Geophysical Research |
| Volume | 90 |
| Issue | B13 |
| Year Published | 1985 |
| Language | English |
| Description | 14 p. |
| First page | 11,275 |
| Last page | 11,288 |
| Google Analytic Metrics | Metrics page |