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- W2129968052 abstract "During eruption, the vent of a Surtseyan volcano is occupied by a highly mobile slurry of tephra, hyaloclastite and water. As magma ascends rapidly through the slurry, mixing occurs due to velocity shear, acceleration of the fluid-fluid contacts and mass incorporation. Consequent expansion of the admixed water causes the jetting and continuous up-rush activity that characterizes Surtseyan volcanism. There is no evidence of the widely accepted fuel-coolant interaction mechanism." @default.
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- W2129968052 date "1983-11-01" @default.
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- W2129968052 title "The mechanism of Surtseyan volcanism" @default.
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- W2129968052 doi "https://doi.org/10.1144/gsjgs.140.6.0939" @default.
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