The control of chamber geometry on triggering volcanic eruptions
The pressure evolution of a cooling and crystallising body of magma stored in the crust is sensitive to the depth and vertical extent of the chamber and also to the volatile content of the magma. In shallow sill-like chambers or in chambers containing magma of high volatile content, the magma become...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
1997
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