Home > Research > Publications & Outputs > Volcano-tectonic interactions as triggers of vo...

Electronic data

  • AG_LW_SL_Reviewed_Manuscript

    Rights statement: This is the author’s version of a work that was accepted for publication in Proceedings of the Geologists' Association. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Proceedings of the Geologists' Association, 126, 6, 2015 DOI: 10.1016/j.pgeola.2015.10.002

    Accepted author manuscript, 565 KB, PDF document

    Available under license: CC BY-NC-ND: Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License

Links

Text available via DOI:

View graph of relations

Volcano-tectonic interactions as triggers of volcanic eruptions

Research output: Contribution to journalJournal article

Published

Standard

Volcano-tectonic interactions as triggers of volcanic eruptions. / Gabrieli, Andrea; Wilson, Lionel; Lane, Stephen John.

In: Proceedings of the Geologists' Association, Vol. 126, No. 6, 12.2015, p. 675-682.

Research output: Contribution to journalJournal article

Harvard

Gabrieli, A, Wilson, L & Lane, SJ 2015, 'Volcano-tectonic interactions as triggers of volcanic eruptions', Proceedings of the Geologists' Association, vol. 126, no. 6, pp. 675-682. https://doi.org/10.1016/j.pgeola.2015.10.002

APA

Vancouver

Author

Gabrieli, Andrea ; Wilson, Lionel ; Lane, Stephen John. / Volcano-tectonic interactions as triggers of volcanic eruptions. In: Proceedings of the Geologists' Association. 2015 ; Vol. 126, No. 6. pp. 675-682.

Bibtex

@article{ff4f928bd9924c60a9786efbb4f488e3,
title = "Volcano-tectonic interactions as triggers of volcanic eruptions",
abstract = "Surface displacements and edifice deformations at active volcanoes can occur when magma reservoirs begin to inflate as new magma enters them. Volcanoes are also subjected to a variety of external lithospheric stresses that are thought to be responsible for triggering volcanic unrest or modifying ongoing activity. However, despite many observations, it is uncertain whether these phenomena can actually interfere with magma chamber dynamics since it is not clear why some volcanoes are more subjected to these interactions than others. In order to determine whether external stresses interfere with volcanic activity, a viscoelastic 3D Finite Element Mogi-based model of Kīlauea volcano's magma chamber was implemented. First, the model was used to replicate an inflation cycle without external stresses. Its results were then compared with the ones obtained if the same model was subjected to tidal stress modulation and a strong (Mw = 7.7) tectonic earthquake. The model showed that tidally-induced pressurization is not sufficiently large to modify the pressure in a 5 km deep volcanic magma chamber, but it suggested how the magma chamber pressure build-up rate can be influenced by tidal pressurization and thus why some volcanoes seem to experience tidal interferences more than others. Furthermore, the model's results suggested why magma chambers are about the same size as calderas both on the Earth and on other Solar System silicate planets. System. Finally, it was used to propose an explanation of why a short-lived eruption at Kīlauea volcano, Hawai’i, began 30 min after the 1975 magnitude 7.7 (Mw) Kalapana earthquake.",
keywords = "Volcanoes, Eruption, Trigger, Stress, FEM, Tides, Earthquakes",
author = "Andrea Gabrieli and Lionel Wilson and Lane, {Stephen John}",
note = "This is the author’s version of a work that was accepted for publication in Proceedings of the Geologists' Association. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Proceedings of the Geologists' Association, 126, 6, 2015 DOI: 10.1016/j.pgeola.2015.10.002",
year = "2015",
month = "12",
doi = "10.1016/j.pgeola.2015.10.002",
language = "English",
volume = "126",
pages = "675--682",
journal = "Proceedings of the Geologists' Association",
number = "6",

}

RIS

TY - JOUR

T1 - Volcano-tectonic interactions as triggers of volcanic eruptions

AU - Gabrieli, Andrea

AU - Wilson, Lionel

AU - Lane, Stephen John

N1 - This is the author’s version of a work that was accepted for publication in Proceedings of the Geologists' Association. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Proceedings of the Geologists' Association, 126, 6, 2015 DOI: 10.1016/j.pgeola.2015.10.002

PY - 2015/12

Y1 - 2015/12

N2 - Surface displacements and edifice deformations at active volcanoes can occur when magma reservoirs begin to inflate as new magma enters them. Volcanoes are also subjected to a variety of external lithospheric stresses that are thought to be responsible for triggering volcanic unrest or modifying ongoing activity. However, despite many observations, it is uncertain whether these phenomena can actually interfere with magma chamber dynamics since it is not clear why some volcanoes are more subjected to these interactions than others. In order to determine whether external stresses interfere with volcanic activity, a viscoelastic 3D Finite Element Mogi-based model of Kīlauea volcano's magma chamber was implemented. First, the model was used to replicate an inflation cycle without external stresses. Its results were then compared with the ones obtained if the same model was subjected to tidal stress modulation and a strong (Mw = 7.7) tectonic earthquake. The model showed that tidally-induced pressurization is not sufficiently large to modify the pressure in a 5 km deep volcanic magma chamber, but it suggested how the magma chamber pressure build-up rate can be influenced by tidal pressurization and thus why some volcanoes seem to experience tidal interferences more than others. Furthermore, the model's results suggested why magma chambers are about the same size as calderas both on the Earth and on other Solar System silicate planets. System. Finally, it was used to propose an explanation of why a short-lived eruption at Kīlauea volcano, Hawai’i, began 30 min after the 1975 magnitude 7.7 (Mw) Kalapana earthquake.

AB - Surface displacements and edifice deformations at active volcanoes can occur when magma reservoirs begin to inflate as new magma enters them. Volcanoes are also subjected to a variety of external lithospheric stresses that are thought to be responsible for triggering volcanic unrest or modifying ongoing activity. However, despite many observations, it is uncertain whether these phenomena can actually interfere with magma chamber dynamics since it is not clear why some volcanoes are more subjected to these interactions than others. In order to determine whether external stresses interfere with volcanic activity, a viscoelastic 3D Finite Element Mogi-based model of Kīlauea volcano's magma chamber was implemented. First, the model was used to replicate an inflation cycle without external stresses. Its results were then compared with the ones obtained if the same model was subjected to tidal stress modulation and a strong (Mw = 7.7) tectonic earthquake. The model showed that tidally-induced pressurization is not sufficiently large to modify the pressure in a 5 km deep volcanic magma chamber, but it suggested how the magma chamber pressure build-up rate can be influenced by tidal pressurization and thus why some volcanoes seem to experience tidal interferences more than others. Furthermore, the model's results suggested why magma chambers are about the same size as calderas both on the Earth and on other Solar System silicate planets. System. Finally, it was used to propose an explanation of why a short-lived eruption at Kīlauea volcano, Hawai’i, began 30 min after the 1975 magnitude 7.7 (Mw) Kalapana earthquake.

KW - Volcanoes

KW - Eruption

KW - Trigger

KW - Stress

KW - FEM

KW - Tides

KW - Earthquakes

U2 - 10.1016/j.pgeola.2015.10.002

DO - 10.1016/j.pgeola.2015.10.002

M3 - Journal article

VL - 126

SP - 675

EP - 682

JO - Proceedings of the Geologists' Association

JF - Proceedings of the Geologists' Association

IS - 6

ER -