Basalto explosivo de aguas profundas en la grieta del arco de Sumisu.

Science (New York, N.Y.)
|June 8, 1990
PubMed
Resumen

Las erupciones volcánicas submarinas de basalto toleiítico crean depósitos únicos de breccia escoriaciosa. El alto contenido de agua magmática impulsa la explosiva actividad volcánica submarina, formando depósitos piroclásticos.

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