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The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift

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The eruptive history and magmatic evolution of Aluto volcano : new insights into silicic peralkaline volcanism in the Ethiopian rift. / Hutchison, William; Pyle, David M.; Mather, Tamsin A.; Yirgu, Gezahegn; Biggs, Juliet; Cohen, Benjamin E.; Barfod, Dan N.; Lewi, Elias.

In: Journal of Volcanology and Geothermal Research, Vol. 328, 15.12.2016, p. 9-33.

Research output: Contribution to journalArticle

Harvard

Hutchison, W, Pyle, DM, Mather, TA, Yirgu, G, Biggs, J, Cohen, BE, Barfod, DN & Lewi, E 2016, 'The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift' Journal of Volcanology and Geothermal Research, vol. 328, pp. 9-33. https://doi.org/10.1016/j.jvolgeores.2016.09.010

APA

Hutchison, W., Pyle, D. M., Mather, T. A., Yirgu, G., Biggs, J., Cohen, B. E., ... Lewi, E. (2016). The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift. Journal of Volcanology and Geothermal Research, 328, 9-33. https://doi.org/10.1016/j.jvolgeores.2016.09.010

Vancouver

Hutchison W, Pyle DM, Mather TA, Yirgu G, Biggs J, Cohen BE et al. The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift. Journal of Volcanology and Geothermal Research. 2016 Dec 15;328:9-33. https://doi.org/10.1016/j.jvolgeores.2016.09.010

Author

Hutchison, William ; Pyle, David M. ; Mather, Tamsin A. ; Yirgu, Gezahegn ; Biggs, Juliet ; Cohen, Benjamin E. ; Barfod, Dan N. ; Lewi, Elias. / The eruptive history and magmatic evolution of Aluto volcano : new insights into silicic peralkaline volcanism in the Ethiopian rift. In: Journal of Volcanology and Geothermal Research. 2016 ; Vol. 328. pp. 9-33.

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@article{a3fe58ca77f344de8914e31e4a14dbdd,
title = "The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift",
abstract = "The silicic peralkaline volcanoes of the East African Rift are some of the least studied volcanoes on Earth. Here we bring together new constraints from fieldwork, remote sensing, geochronology and geochemistry to present the first detailed account of the eruptive history of Aluto, a restless silicic volcano located in a densely populated section of the Main Ethiopian Rift. Prior to the growth of the Aluto volcanic complex (before 500 ka) the region was characterized by a significant period of fault development and mafic fissure eruptions. The earliest volcanism at Aluto built up a trachytic complex over 8 km in diameter. Aluto then underwent large-volume ignimbrite eruptions at 316 ± 19 ka and 306 ± 12 ka developing a ~ 42 km2 collapse structure. After a hiatus of ~ 250 ka, a phase of post-caldera volcanism initiated at 55 ± 19 ka and the most recent eruption of Aluto has a radiocarbon age of 0.40 ± 0.05 cal. ka BP. During this post-caldera phase highly-evolved peralkaline rhyolite lavas, ignimbrites and pumice fall deposits have erupted from vents across the complex. Geochemical modelling is consistent with rhyolite genesis from protracted fractionation (> 80{\%}) of basalt that is compositionally similar to rift-related basalts found east of the complex. Based on the style and volume of recent eruptions we suggest that silicic eruptions occur at an average rate of 1 per 1000 years, and that future eruptions of Aluto will involve explosive emplacement of localised pumice cones and effusive obsidian coulees of volumes in the range 1–100 × 106 m3.",
keywords = "Eruptive history, Geothermal resources, Main Ethiopian Rift, Peralkaline, Silicic volcanism, Volcanic hazard",
author = "William Hutchison and Pyle, {David M.} and Mather, {Tamsin A.} and Gezahegn Yirgu and Juliet Biggs and Cohen, {Benjamin E.} and Barfod, {Dan N.} and Elias Lewi",
note = "W.H., D.M.P., T.A.M. and J.B. are supported by and contribute to the NERC Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET). W.H. was funded by NERC studentship, NE/J5000045/1. Additional funding for the project was provided by: University College and the Department of Zoology (Boise Trust Fund) at the University of Oxford, as well as the Geological Remote Sensing Group, the Edinburgh Geological Society and the Leverhulme Trust.",
year = "2016",
month = "12",
day = "15",
doi = "10.1016/j.jvolgeores.2016.09.010",
language = "English",
volume = "328",
pages = "9--33",
journal = "Journal of Volcanology and Geothermal Research",
issn = "0377-0273",
publisher = "Elsevier",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - The eruptive history and magmatic evolution of Aluto volcano

T2 - Journal of Volcanology and Geothermal Research

AU - Hutchison, William

AU - Pyle, David M.

AU - Mather, Tamsin A.

AU - Yirgu, Gezahegn

AU - Biggs, Juliet

AU - Cohen, Benjamin E.

AU - Barfod, Dan N.

AU - Lewi, Elias

N1 - W.H., D.M.P., T.A.M. and J.B. are supported by and contribute to the NERC Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET). W.H. was funded by NERC studentship, NE/J5000045/1. Additional funding for the project was provided by: University College and the Department of Zoology (Boise Trust Fund) at the University of Oxford, as well as the Geological Remote Sensing Group, the Edinburgh Geological Society and the Leverhulme Trust.

PY - 2016/12/15

Y1 - 2016/12/15

N2 - The silicic peralkaline volcanoes of the East African Rift are some of the least studied volcanoes on Earth. Here we bring together new constraints from fieldwork, remote sensing, geochronology and geochemistry to present the first detailed account of the eruptive history of Aluto, a restless silicic volcano located in a densely populated section of the Main Ethiopian Rift. Prior to the growth of the Aluto volcanic complex (before 500 ka) the region was characterized by a significant period of fault development and mafic fissure eruptions. The earliest volcanism at Aluto built up a trachytic complex over 8 km in diameter. Aluto then underwent large-volume ignimbrite eruptions at 316 ± 19 ka and 306 ± 12 ka developing a ~ 42 km2 collapse structure. After a hiatus of ~ 250 ka, a phase of post-caldera volcanism initiated at 55 ± 19 ka and the most recent eruption of Aluto has a radiocarbon age of 0.40 ± 0.05 cal. ka BP. During this post-caldera phase highly-evolved peralkaline rhyolite lavas, ignimbrites and pumice fall deposits have erupted from vents across the complex. Geochemical modelling is consistent with rhyolite genesis from protracted fractionation (> 80%) of basalt that is compositionally similar to rift-related basalts found east of the complex. Based on the style and volume of recent eruptions we suggest that silicic eruptions occur at an average rate of 1 per 1000 years, and that future eruptions of Aluto will involve explosive emplacement of localised pumice cones and effusive obsidian coulees of volumes in the range 1–100 × 106 m3.

AB - The silicic peralkaline volcanoes of the East African Rift are some of the least studied volcanoes on Earth. Here we bring together new constraints from fieldwork, remote sensing, geochronology and geochemistry to present the first detailed account of the eruptive history of Aluto, a restless silicic volcano located in a densely populated section of the Main Ethiopian Rift. Prior to the growth of the Aluto volcanic complex (before 500 ka) the region was characterized by a significant period of fault development and mafic fissure eruptions. The earliest volcanism at Aluto built up a trachytic complex over 8 km in diameter. Aluto then underwent large-volume ignimbrite eruptions at 316 ± 19 ka and 306 ± 12 ka developing a ~ 42 km2 collapse structure. After a hiatus of ~ 250 ka, a phase of post-caldera volcanism initiated at 55 ± 19 ka and the most recent eruption of Aluto has a radiocarbon age of 0.40 ± 0.05 cal. ka BP. During this post-caldera phase highly-evolved peralkaline rhyolite lavas, ignimbrites and pumice fall deposits have erupted from vents across the complex. Geochemical modelling is consistent with rhyolite genesis from protracted fractionation (> 80%) of basalt that is compositionally similar to rift-related basalts found east of the complex. Based on the style and volume of recent eruptions we suggest that silicic eruptions occur at an average rate of 1 per 1000 years, and that future eruptions of Aluto will involve explosive emplacement of localised pumice cones and effusive obsidian coulees of volumes in the range 1–100 × 106 m3.

KW - Eruptive history

KW - Geothermal resources

KW - Main Ethiopian Rift

KW - Peralkaline

KW - Silicic volcanism

KW - Volcanic hazard

U2 - 10.1016/j.jvolgeores.2016.09.010

DO - 10.1016/j.jvolgeores.2016.09.010

M3 - Article

VL - 328

SP - 9

EP - 33

JO - Journal of Volcanology and Geothermal Research

JF - Journal of Volcanology and Geothermal Research

SN - 0377-0273

ER -

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ID: 248865167