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Permeable convection above magma bodies—discussion

Authors
Journal
Tectonophysics
0040-1951
Publisher
Elsevier
Publication Date
Volume
95
Identifiers
DOI: 10.1016/0040-1951(83)90078-1

Abstract

Abstract Thermal two phases permeable convection in the cooled layer, at the top of a former lava lake, is limited by the amount of water available or by the rate of surface cooling, not by permeability. Two phases convection at depth must take into account the actual properties of steam.

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