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dc.contributor.authorHutchison, William
dc.contributor.authorMather, Tamsin A.
dc.contributor.authorPyle, David M.
dc.contributor.authorBiggs, Juliet
dc.contributor.authorYirgu, Gezahegn
dc.date.accessioned2017-10-25T12:30:12Z
dc.date.available2017-10-25T12:30:12Z
dc.date.issued2015-06-01
dc.identifier.citationHutchison , W , Mather , T A , Pyle , D M , Biggs , J & Yirgu , G 2015 , ' Structural controls on fluid pathways in an active rift system : a case study of the Aluto volcanic complex ' Geosphere , vol. 11 , no. 3 , pp. 542-562 . https://doi.org/10.1130/GES01119.1en
dc.identifier.issn1553-040X
dc.identifier.otherPURE: 245804207
dc.identifier.otherPURE UUID: c8077b46-75f8-4e35-b577-2b98a1648e60
dc.identifier.otherWOS: 000359479400002
dc.identifier.otherScopus: 84936126839
dc.identifier.urihttp://hdl.handle.net/10023/11918
dc.descriptionHutchison was funded by NERC studentship NE/J5000045/1.en
dc.description.abstractIn volcanically and seismically active rift systems, preexisting faults may control the rise and eruption of magma, and direct the flow of hydrothermal fluids and gas in the subsurface. Using high-resolution airborne imagery, field observations, and CO2 degassing data on Aluto, a typical young silicic volcano in the Main Ethiopian Rift, we explore how preexisting tectonic and volcanic structures control fluid pathways and spatial patterns of volcanism, hydrothermal alteration and degassing. A new light detection and ranging (lidar) digital elevation model and evidence from deep geothermal wells show that the Aluto volcanic complex is dissected by rift-related extensional faults with throws of 50-100 m. Mapping of volcanic vent distributions reveals a structural control by either rift-aligned faults or an elliptical caldera ring fracture. Soil-gas CO2 degassing surveys show elevated fluxes (>>100 g m-2 d-1) along major faults and volcanic structures, but significant variations in CO2 flux along the fault zones reflect differences in near-surface permeability caused by changes in topography and surface lithology. The CO2 emission from an active geothermal area adjacent to the major fault scarp of Aluto amounted to similar to 60 t d-1; we estimate the total CO2 emission from Aluto to be 250-500 t d-1. Preexisting volcanic and tectonic structures have played a key role in the development of the Aluto volcanic complex and continue to facilitate the expulsion of gases and geothermal fluids. This case study emphasizes the importance of structural mapping on active rift volcanoes to understand the geothermal field as well as potential volcanic hazards.
dc.format.extent21
dc.language.isoeng
dc.relation.ispartofGeosphereen
dc.rights© 2015 Geological Society of America. Gold Open Access: This paper is published under the terms of the CC-BY license.en
dc.subjectMain-Ethiopian-riften
dc.subjectLangano geothermal-fielden
dc.subjectCarbon-dioxide emissionsen
dc.subjectPoint-like featuresen
dc.subjectSoil CO2 fluxen
dc.subjectDiffuse emissionen
dc.subjectNew Zealanden
dc.subjectMt. Etnaen
dc.subjectHydrothermal alterationen
dc.subjectVolatile emissionsen
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleStructural controls on fluid pathways in an active rift system : a case study of the Aluto volcanic complexen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.School of Earth & Environmental Sciencesen
dc.identifier.doihttps://doi.org/10.1130/GES01119.1
dc.description.statusPeer revieweden


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