Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics
The quantification of timing for crystallization and exsolution processes are fundamental to our understanding of basaltic magma ascent dynamics. Here, the authors constrain timings to show that plagioclase reaches equilibrium in 1-2 hours, whereas ascent times were <1 hour.
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2016-12-01
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| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms13402 |
| _version_ | 1818978527996805120 |
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| author | G. La Spina M. Burton M. de’ Michieli Vitturi F. Arzilli |
| author_facet | G. La Spina M. Burton M. de’ Michieli Vitturi F. Arzilli |
| author_sort | G. La Spina |
| collection | DOAJ |
| description | The quantification of timing for crystallization and exsolution processes are fundamental to our understanding of basaltic magma ascent dynamics. Here, the authors constrain timings to show that plagioclase reaches equilibrium in 1-2 hours, whereas ascent times were <1 hour. |
| first_indexed | 2024-12-20T16:45:04Z |
| format | Article |
| id | doaj.art-94a22e7fd6e84b63be1e081fe3d731fc |
| institution | Directory Open Access Journal |
| issn | 2041-1723 |
| language | English |
| last_indexed | 2024-12-20T16:45:04Z |
| publishDate | 2016-12-01 |
| publisher | Nature Portfolio |
| record_format | Article |
| series | Nature Communications |
| spelling | doaj.art-94a22e7fd6e84b63be1e081fe3d731fc2022-12-21T19:32:57ZengNature PortfolioNature Communications2041-17232016-12-017111010.1038/ncomms13402Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamicsG. La Spina0M. Burton1M. de’ Michieli Vitturi2F. Arzilli3School of Earth and Environmental Sciences, The University of ManchesterSchool of Earth and Environmental Sciences, The University of ManchesterIstituto Nazionale di Geofisica e VulcanologiaSchool of Earth and Environmental Sciences, The University of ManchesterThe quantification of timing for crystallization and exsolution processes are fundamental to our understanding of basaltic magma ascent dynamics. Here, the authors constrain timings to show that plagioclase reaches equilibrium in 1-2 hours, whereas ascent times were <1 hour.https://doi.org/10.1038/ncomms13402 |
| spellingShingle | G. La Spina M. Burton M. de’ Michieli Vitturi F. Arzilli Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics Nature Communications |
| title | Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics |
| title_full | Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics |
| title_fullStr | Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics |
| title_full_unstemmed | Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics |
| title_short | Role of syn-eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics |
| title_sort | role of syn eruptive plagioclase disequilibrium crystallization in basaltic magma ascent dynamics |
| url | https://doi.org/10.1038/ncomms13402 |
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