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Evidence for the formation of silicic lava by pyroclast sintering

Evidence for the formation of silicic lava by pyroclast sintering

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_64aa01c778634760add89e9397ad9c61

Evidence for the formation of silicic lava by pyroclast sintering

About this item

Full title

Evidence for the formation of silicic lava by pyroclast sintering

Publisher

London: Nature Publishing Group UK

Journal title

Nature communications, 2024-06, Vol.15 (1), p.5347-10, Article 5347

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

Contents

Silicic lavas can be produced by the sintering of pyroclasts in the volcanic sub-surface, and then advected out of the vent. Here, we provide evidence for this mechanism preserved in the exposed post-glacial remnants of a silicic volcanic conduit at Hrafntinnuhryggur, Krafla volcano, Iceland. We show that the conduit margins are a clast-supported p...

Alternative Titles

Full title

Evidence for the formation of silicic lava by pyroclast sintering

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_64aa01c778634760add89e9397ad9c61

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_64aa01c778634760add89e9397ad9c61

Other Identifiers

ISSN

2041-1723

E-ISSN

2041-1723

DOI

10.1038/s41467-024-49601-6

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