Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption

Pink and white raft pumice from the 2012 Havre deep-sea eruption experienced prolonged high-temperature atmospheric oxidation of magnetite to hematite which suggests a short but powerful explosive phase, according to microanalytical investigation.

Bibliographic Details
Main Authors: Joseph Knafelc, Scott E. Bryan, Michael W. M. Jones, David Gust, Guil Mallmann, Henrietta E. Cathey, Andrew J. Berry, Eric C. Ferré, Daryl L. Howard
Format: Article
Language:English
Published: Nature Portfolio 2022-02-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-022-00355-3
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author Joseph Knafelc
Scott E. Bryan
Michael W. M. Jones
David Gust
Guil Mallmann
Henrietta E. Cathey
Andrew J. Berry
Eric C. Ferré
Daryl L. Howard
author_facet Joseph Knafelc
Scott E. Bryan
Michael W. M. Jones
David Gust
Guil Mallmann
Henrietta E. Cathey
Andrew J. Berry
Eric C. Ferré
Daryl L. Howard
author_sort Joseph Knafelc
collection DOAJ
description Pink and white raft pumice from the 2012 Havre deep-sea eruption experienced prolonged high-temperature atmospheric oxidation of magnetite to hematite which suggests a short but powerful explosive phase, according to microanalytical investigation.
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spelling doaj.art-f083cb1c369b4ecfa3b4053b5ef77c2e2022-12-22T01:35:23ZengNature PortfolioCommunications Earth & Environment2662-44352022-02-013111110.1038/s43247-022-00355-3Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruptionJoseph Knafelc0Scott E. Bryan1Michael W. M. Jones2David Gust3Guil Mallmann4Henrietta E. Cathey5Andrew J. Berry6Eric C. Ferré7Daryl L. Howard8School of Earth & Atmospheric Sciences, Queensland University of TechnologySchool of Earth & Atmospheric Sciences, Queensland University of TechnologyCentral Analytical Research Facility, Queensland University of TechnologySchool of Earth & Atmospheric Sciences, Queensland University of TechnologyResearch School of Earth Sciences, Australian National UniversitySchool of Earth & Atmospheric Sciences, Queensland University of TechnologyResearch School of Earth Sciences, Australian National UniversitySchool of Geosciences, University of Louisiana at LafayetteAustralian Synchrotron, ANSTOPink and white raft pumice from the 2012 Havre deep-sea eruption experienced prolonged high-temperature atmospheric oxidation of magnetite to hematite which suggests a short but powerful explosive phase, according to microanalytical investigation.https://doi.org/10.1038/s43247-022-00355-3
spellingShingle Joseph Knafelc
Scott E. Bryan
Michael W. M. Jones
David Gust
Guil Mallmann
Henrietta E. Cathey
Andrew J. Berry
Eric C. Ferré
Daryl L. Howard
Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption
Communications Earth & Environment
title Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption
title_full Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption
title_fullStr Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption
title_full_unstemmed Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption
title_short Havre 2012 pink pumice is evidence of a short-lived, deep-sea, magnetite nanolite-driven explosive eruption
title_sort havre 2012 pink pumice is evidence of a short lived deep sea magnetite nanolite driven explosive eruption
url https://doi.org/10.1038/s43247-022-00355-3
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