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Traversing nature's danger zone: getting up close with Sumatra's volcanoes
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Berggrundsgeologi.
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper, Berggrundsgeologi.
Scripps Institution of Oceanography, University of California San Diego, California, USA.
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Roma, Italy.
Visa övriga samt affilieringar
2012 (Engelska)Ingår i: Geology Today, ISSN 0266-6979, E-ISSN 1365-2451, Vol. 28, nr 2, s. 64-70Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

The Indonesian island of Sumatra, located in one of the most active zones of the Pacific Ring of Fire, is characterized by a chain of subduction-zone volcanoes which extend the entire length of the island. As a group of volcanic geochemists, we embarked upon a five-week sampling expedition to these exotic, remote, and in part explosive volcanoes (SAGE 2010; Sumatran Arc Geochemical Expedition). We set out to collect rock and gas samples from 17 volcanic centres from the Sumatran segment of the Sunda arc system, with the aim of obtaining a regionally significant sample set that will allow quantification of the respective roles of mantle versus crustal sources to magma genesis along the strike of the arc. Here we document our geological journey through Sumatra's unpredictable terrain, including the many challenges faced when working on active volcanoes in pristine tropical climes.

Ort, förlag, år, upplaga, sidor
2012. Vol. 28, nr 2, s. 64-70
Nationell ämneskategori
Geovetenskap och miljövetenskap
Forskningsämne
Geovetenskap med inriktning mot mineralogi, petrologi och tektonik
Identifikatorer
URN: urn:nbn:se:uu:diva-188509DOI: 10.1111/j.1365-2451.2012.00828.xOAI: oai:DiVA.org:uu-188509DiVA, id: diva2:578018
Tillgänglig från: 2012-12-17 Skapad: 2012-12-17 Senast uppdaterad: 2017-12-06Bibliografiskt granskad
Ingår i avhandling
1. Characterising volcanic magma plumbing systems: A tool to improve eruption forecasting at hazardous volcanoes
Öppna denna publikation i ny flik eller fönster >>Characterising volcanic magma plumbing systems: A tool to improve eruption forecasting at hazardous volcanoes
2015 (Engelska)Doktorsavhandling, sammanläggning (Övrigt vetenskapligt)
Abstract [en]

This thesis attempts to develop our understanding of volcanic magma plumbing systems and the magmatic processes that operate within them, such as fractional crystallisation, crustal partial melting, assimilation, and magma mixing. I utilise petrology, rock and mineral geochemistry, and isotope systematics to seek to improve our ability to forecast the eruptive frequency and style of active volcanoes, an aspect often lacking in current volcano monitoring efforts. In particular, magma reservoir dynamics are investigated from a mineral scale at Katla volcano in Iceland, to a sub-mineral scale at Merapi, Kelud, and Toba volcanoes in Indonesia.

The magma plumbing architecture of Katla volcano on Iceland is explored in the first part of this thesis. Crystalline components within tephra and volcanic rock preserve a record of the physical and chemical evolution of a magma, and are analysed through oxygen isotopic and thermobarometric techniques to temporally constrain changes in reservoir depth and decode the petrogenesis of the lavas. We find both prolonged upper crustal magma storage and shallow level assimilation to be occurring at Katla. The results generated from combining these analytical strands reveal the potential for unpredictable explosive volcanism at this lively Icelandic volcano.

The second part of this thesis examines the magma plumbing systems of Merapi, Kelud and Toba volcanoes of the Sunda arc in Indonesia at higher temporal and petrological resolution than possible for Katla (e.g., due to the crystal poor character of the rocks). For this part of the thesis, minerals were analysed in-situ to take advantage of sub-crystal scale isotopic variations in order to investigate processes of shallow-level assimilation in the build-up to particular eruptions. We find that intra-crystal analyses reveal an otherwise hidden differentiation history at these volcanoes, and establish a better understanding as to how they may have rapidly achieved a critical explosive state.

The outcomes of this thesis therefore deepen our knowledge of evolutionary trends in magma plumbing system dynamics, and highlight the importance of understanding the geochemical processes that can prime a volcano for eruption. Lastly, I emphasise the vital contribution petrology can make in current volcano monitoring efforts. 

Ort, förlag, år, upplaga, sidor
Uppsala: Acta Universitatis Upsaliensis, 2015. s. 42
Serie
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology, ISSN 1651-6214 ; 1325
Nyckelord
magma plumbing, oxygen isotopes, thermobarometry, crustal assimilation, Katla, Merapi, Kelud, Toba, volcanic hazards
Nationell ämneskategori
Geologi
Forskningsämne
Geovetenskap med inriktning mot mineralogi, petrologi och tektonik
Identifikatorer
urn:nbn:se:uu:diva-267473 (URN)978-91-554-9424-7 (ISBN)
Disputation
2016-01-22, Hambergsalen, Geocentrum, Villavägen 16, Uppsala, 10:00 (Engelska)
Opponent
Handledare
Tillgänglig från: 2015-12-17 Skapad: 2015-11-23 Senast uppdaterad: 2016-01-13

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Budd, David A.Troll, Valentin R.Jolis, Ester M.

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