Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards
Silicic magma in the shallow crust has the potential to violently erupt, depending on its ability to release overpressures caused by magmatic volatiles (outgassing). Deformation-induced outgassing is prevalent along volcanic conduit margins, where ascending magma is sheared at high rates. However, t...
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Uppsala universitet, Mineralogi, petrologi och tektonik
2024
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ftuppsalauniv:oai:DiVA.org:uu-524861 2024-05-19T07:43:00+00:00 Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards Witcher, Taylor 2024 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-524861 eng eng Uppsala universitet, Mineralogi, petrologi och tektonik Uppsala Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology, 1651-6214 2380 orcid:0000-0002-4326-3607 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-524861 urn:isbn:978-91-513-2080-9 info:eu-repo/semantics/openAccess magma deformation magmatic outgassing magmatic intrusions rhyolite Sandfell laccolith crystal mush volcanic hazards Geology Geologi Doctoral thesis, comprehensive summary info:eu-repo/semantics/doctoralThesis text 2024 ftuppsalauniv 2024-04-23T23:36:54Z Silicic magma in the shallow crust has the potential to violently erupt, depending on its ability to release overpressures caused by magmatic volatiles (outgassing). Deformation-induced outgassing is prevalent along volcanic conduit margins, where ascending magma is sheared at high rates. However, this mechanism limits outgassing to the contact with the host rock, leaving the bulk of the magma untouched and full of volatiles. This thesis presents a different mechanism of silicic outgassing that affects the interior volume of a magma body as well as the margins. Here, we present a case study of deformation features within the Miocene Sandfell laccolith, Eastern Iceland: a 0.57 km3 dome-shaped rhyolitic magma body with ~5 vol% phenocrysts and a microcrystalline groundmass. Similar textures have been reported in lava domes and intrusions with various compositions and crystallinities. The range of deformation features are 1. porous flow bands, 2. elongated pores within flow bands, 3. 1–5 cm long tensile fractures aligned in bands, 4. 5–20 cm fractures within bands (often multiple fracture sets), and 5. breccia (densely spaced bands that are no longer distinguishable). The bands in each category range in length from ‘lenses’ (~15 cm) to laterally expansive (several meters), and usually taper at the tips. The bands are interlayered with coherent, undeformed rhyolite, and their morphology varies between planar, undulating, and anastomosing. The chapters within this thesis characterize the spatial distribution of each stage of ‘fracture banding’ and interpret their role in magma emplacement (Paper I); analyze the textures of each deformation stage on a micro-scale to interpret the rheology of the magma during formation (Paper II); investigate the mineral assemblage of fracture fillings and apply results to metal separation from parent magma in early ore systems (Paper III); and attempt to experimentally recreate fracture bands in a laboratory setting (Paper IV). The results of these chapters suggest the ... Doctoral or Postdoctoral Thesis Iceland Uppsala University: Publications (DiVA) |
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Uppsala University: Publications (DiVA) |
op_collection_id |
ftuppsalauniv |
language |
English |
topic |
magma deformation magmatic outgassing magmatic intrusions rhyolite Sandfell laccolith crystal mush volcanic hazards Geology Geologi |
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magma deformation magmatic outgassing magmatic intrusions rhyolite Sandfell laccolith crystal mush volcanic hazards Geology Geologi Witcher, Taylor Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards |
topic_facet |
magma deformation magmatic outgassing magmatic intrusions rhyolite Sandfell laccolith crystal mush volcanic hazards Geology Geologi |
description |
Silicic magma in the shallow crust has the potential to violently erupt, depending on its ability to release overpressures caused by magmatic volatiles (outgassing). Deformation-induced outgassing is prevalent along volcanic conduit margins, where ascending magma is sheared at high rates. However, this mechanism limits outgassing to the contact with the host rock, leaving the bulk of the magma untouched and full of volatiles. This thesis presents a different mechanism of silicic outgassing that affects the interior volume of a magma body as well as the margins. Here, we present a case study of deformation features within the Miocene Sandfell laccolith, Eastern Iceland: a 0.57 km3 dome-shaped rhyolitic magma body with ~5 vol% phenocrysts and a microcrystalline groundmass. Similar textures have been reported in lava domes and intrusions with various compositions and crystallinities. The range of deformation features are 1. porous flow bands, 2. elongated pores within flow bands, 3. 1–5 cm long tensile fractures aligned in bands, 4. 5–20 cm fractures within bands (often multiple fracture sets), and 5. breccia (densely spaced bands that are no longer distinguishable). The bands in each category range in length from ‘lenses’ (~15 cm) to laterally expansive (several meters), and usually taper at the tips. The bands are interlayered with coherent, undeformed rhyolite, and their morphology varies between planar, undulating, and anastomosing. The chapters within this thesis characterize the spatial distribution of each stage of ‘fracture banding’ and interpret their role in magma emplacement (Paper I); analyze the textures of each deformation stage on a micro-scale to interpret the rheology of the magma during formation (Paper II); investigate the mineral assemblage of fracture fillings and apply results to metal separation from parent magma in early ore systems (Paper III); and attempt to experimentally recreate fracture bands in a laboratory setting (Paper IV). The results of these chapters suggest the ... |
format |
Doctoral or Postdoctoral Thesis |
author |
Witcher, Taylor |
author_facet |
Witcher, Taylor |
author_sort |
Witcher, Taylor |
title |
Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards |
title_short |
Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards |
title_full |
Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards |
title_fullStr |
Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards |
title_full_unstemmed |
Viscous-brittle deformation of shallowly emplaced silicic magma : Implications for outgassing and volcanic hazards |
title_sort |
viscous-brittle deformation of shallowly emplaced silicic magma : implications for outgassing and volcanic hazards |
publisher |
Uppsala universitet, Mineralogi, petrologi och tektonik |
publishDate |
2024 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-524861 |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology, 1651-6214 2380 orcid:0000-0002-4326-3607 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-524861 urn:isbn:978-91-513-2080-9 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1799482710453911552 |