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VESPER SIGNED

Volcanoes: eruptive style, pre-eruptive evolution and risk

Total Cost €

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EC-Contrib. €

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Partnership

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 VESPER project word cloud

Explore the words cloud of the VESPER project. It provides you a very rough idea of what is the project "VESPER" about.

mitigate    constraints       volcanoes    constrained    jvolgeores    dissolved    gt    structure    plate    shock    place    04    crystal    experimental    02    composition    natural    style    last    inherited    longer    patchy    suitable    cf    1007    storage    75    mapping    eruptive    2016    montero    island    plumbing    magma    relation    permit    chamberlain    predict    context    nature    age    million    erupted    chemistry    014    gertisser    description    preece    hazards    texture    data    understand    magmas    clear    2013    mixing    geochemical    1016    risks    s00445    rocks    eruptions    events    al    subduction    identification    revealed    bea    crystals    explosive    ascension    sub    deposits    herd    016    few    isotopic    assimilated    pb    compositions    periodicity    006    magmatic    zoning    barclay    chemgeo    suffer    event    obtain    et    active    prior    survive    zircon    mineral    zircons    numerical    eruption    doi    relationship    aerial    references    volcanic    thermal    ages    effusive    rock    cargoes   

Project "VESPER" data sheet

The following table provides information about the project.

Coordinator
UNIVERSITY OF EAST ANGLIA 

Organization address
address: EARLHAM ROAD
city: NORWICH
postcode: NR4 7TJ
website: http://www.uea.ac.uk

contact info
title: n.a.
name: n.a.
surname: n.a.
function: n.a.
email: n.a.
telephone: n.a.
fax: n.a.

 Coordinator Country United Kingdom [UK]
 Total cost 195˙454 €
 EC max contribution 195˙454 € (100%)
 Programme 1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
 Code Call H2020-MSCA-IF-2016
 Funding Scheme MSCA-IF-EF-ST
 Starting year 2018
 Duration (year-month-day) from 2018-02-19   to  2020-02-18

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    UNIVERSITY OF EAST ANGLIA UK (NORWICH) coordinator 195˙454.00

Map

 Project objective

This project will use the compositions and crystal cargoes of erupted magmas to study pre-eruptive behaviour of magmatic systems. The aim is to understand their relationship to, and control on, periodicity and style of volcanic eruptions to mitigate hazards and risks. To do this we will undertake detailed description of the whole-rock composition and mineral chemistry of volcanic rocks from active intra-plate and subduction-related volcanoes. New knowledge about zircon behaviour will then be considered in the context of these well-constrained systems.

Experimental and numerical modelling predict pre-existing zircons that survive being dissolved in magmas suffer thermal shock that affects their structure, patchy zoning, and U-Th-Pb isotopic system i.e., ages (1). We shall analyse the texture and composition of inherited, assimilated and magmatic zircons. Study of these natural volcanic zircons will place constraints on experimental and modelling thermal shock results and permit identification of crystals suitable for analysis to obtain reliable age information.

Recent detailed field mapping of volcanic deposits on intra-plate Ascension Island, for example, has revealed >75 explosive and >40 effusive sub-aerial eruptions in the last million years. Only a few of these show clear evidence for magma mixing prior to eruption. We will use zircon and whole-rock geochemical data to understand the nature of these and other pre-eruptive processes.

Our main objective is to obtain information about magma storage conditions and plumbing systems in relation to effusive and explosive volcanic activity (cf., 2, 3). Such information may be used to consider future behaviour and so possible short-term, within event, and longer term, between events, potential risks.

References 1. Bea F., Montero P. 2013. doi: 10.1016/j.chemgeo.2013.04.014 2. Preece K., Barclay J., Gertisser R., Herd R. 2013. doi: 10.1016/j.jvolgeores.2013.02.006 3. Chamberlain et al. 2016. doi: 10.1007/s00445-016-1

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