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- W232526271 abstract "Extrusive submarine volcanism must be influenced by magma–water interaction. In the continental areas, due to groundwater and hydrous fluids, uprising magma frequently interacts with water. The major effect of magma–water interaction is an increase in thermal energy flux and induction of a special type of magma fragmentation, i.e., phreatomagmatic fragmentation. The products of this process are typical and discriminative: angular, blocky particles with diameters between 30 and 130 μm, and peculiar surface textures. Intensities of magma–water interaction strongly depend on the material and environmental parameters and on the contact dynamics. They range from mild effusion to extremely destructive explosive pulses." @default.
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- W232526271 date "2015-01-01" @default.
- W232526271 modified "2023-10-01" @default.
- W232526271 title "Magma–Water Interaction and Phreatomagmatic Fragmentation" @default.
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- W232526271 doi "https://doi.org/10.1016/b978-0-12-385938-9.00026-2" @default.
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