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.
Main Authors: | , , , , , , , , |
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Format: | Article |
Language: | English |
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Nature Portfolio
2022-02-01
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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. |
first_indexed | 2024-12-10T20:06:50Z |
format | Article |
id | doaj.art-f083cb1c369b4ecfa3b4053b5ef77c2e |
institution | Directory Open Access Journal |
issn | 2662-4435 |
language | English |
last_indexed | 2024-12-10T20:06:50Z |
publishDate | 2022-02-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Communications Earth & Environment |
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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