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  5. Dynamic plumbing system beneath volcanoes revealed by kinetic modeling, and the connection to monitoring data: An example from Mt. Etna
 
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Dynamic plumbing system beneath volcanoes revealed by kinetic modeling, and the connection to monitoring data: An example from Mt. Etna

Author(s)
Kahl, M.  
Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität, Bochum, Bochum 44780, Germany  
Chakraborty, S.  
Institut für Geologie, Mineralogie & Geophysik, Ruhr-Universität, Bochum, Bochum 44780, Germany  
Costa, F.  
Earth Observatory of Singapore, Nanyang Technological University, Singapore 639798, Singapore  
Pompilio, M.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia  
Language
English
Obiettivo Specifico
1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
2.3. TTC - Laboratori di chimica e fisica delle rocce
3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Earth and Planetary Science Letters  
Issue/vol(year)
1-2/308(2011)
Publisher
Elsevier
Pages (printed)
11-22
Date Issued
August 1, 2011
DOI
10.1016/j.epsl.2011.05.008
Alternative Location
http://www.sciencedirect.com/science/article/pii/S0012821X11002792
URI
https://www.earth-prints.org/handle/2122/7497
Subjects
04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology  
04. Solid Earth::04.08. Volcanology::04.08.03. Magmas  
04. Solid Earth::04.08. Volcanology::04.08.05. Volcanic rocks  
Subjects

Etna

plumbing system

olivine

zoning

timescales

monitoring

Abstract
Our ability to monitor volcanoes (using seismic signals, ground deformation, gas fluxes, or other ground and satellite based observations) as well as our understanding of melt reservoirs that feed eruptions have evolved tremendously in recent years. The complex plumbing systems that are thought to feed eruptions are, however, difficult to relate to the monitoring signals. Here we show that the record preserved in compositional zoning of erupted minerals may be used to reconstruct sections of the plumbing system. Kinetic modeling of such zoning can yield information on the residence time of magma in different segments of the plumbing systems. This allows a more nuanced evaluation of the link between observed monitoring signals or eruption styles and the magmatic processes and movement of batches of melts at depth. The approach is illustrated through a study of the compositional zoning recorded in olivine crystals from the 1991–1993 SE-flank eruption products of Mt. Etna (Sicily). The zoning patterns in crystals reveal that the plumbing system of the volcano consisted of at least three different magmatic environments between which magma was transported and mixed in the year or two preceding the start of eruption. Quantification of this history indicates that two main pathways of melt migration and three timescales dominated the dynamics of the system. Combination of this information with the timing of observation of various monitoring signals allows a reconstruction of the dynamic evolution of this section of the plumbing system during the early stages of the 1991–1993 eruption. It is seen, for example, how the migration of melt through the same sections of the plumbing system can cause pre-eruptive triggering, enhance Strombolian activity, and through the ensuing eruption cleanse and flush the plumbing system. Different kinds of mixing occur simultaneously at different sections of the plumbing system on different timescales (a few days up to two years).
Type
article
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