Relationship between eruptive style and vesicularity of juvenile clasts during eruptive episode A of Towada Volcano, Northeast Japan
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文摘

We compared the ejecta vesicularity between magmatic and phreatomagmatic phases.

Vesicularity discrepancy between lapilli and shard is caused by the time of quenched.

Phreatoplinian products are good to estimate the primary vesicularity in a conduit.

Bubble expansion is considered as important factor causing phreatoplinian eruption.

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