Counter-current convection in a volcanic conduit
Volcanoes of Strombolian type are able to maintain their semi-permanent eruptive states through the constant convective recycling of magma within the conduit leading from the magma chamber. In this paper we study the form of this convection using an analytic model of degassing two-phase flow in a ve...
| المؤلفون الرئيسيون: | , |
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| التنسيق: | Journal article |
| منشور في: |
Elsevier
2018
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