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On the thermal viability of dikes leaving magma chambers
Allan M. Rubin
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peer-review
70
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Keyphrases
Magma Chamber
100%
Magma
42%
Solidus
28%
Magma Temperature
28%
Rhyolite
28%
Solidus Temperature
14%
Basaltic Dikes
14%
Magma Source
14%
Dike Propagation
14%
Earth and Planetary Sciences
Magma Chamber
100%
Magma
66%
Rhyolite
22%
Propagation Velocity
11%