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  • A complex phreatomagmatic volcano in the Pannonian Basin (Tihany paleovolcano, Hungary)
  • . This is the main volcanic structure of peninsula and phreatomagmatic activity probably began here. The lapilli and coarse ashes in the pyroclastites are generally mud-coated, accretionary lapilli are common, and the tuffs are frequently light brownish, suggesting
  • The morphology and origin of wide craters at Al Haruj al Abyad, Libya : maars and phreatomagmatism in a large intracontinental flood lava field?
  • Three regional tectonic phases can be distinguished during the past million years: 1. formation of a large graben, 2. sinking of segments of the volcano complex, 3. faulting, accompanied by phreatomagmatic volcanism. Each event was followed by small
  • was derived from phreatomagmatic eruptions partially with additional proportions of rock fragments from local lava flows. Grain shape and size indicate the materials were transported by aeolian processes rather than by fluvial processes. A spectral