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VESPER SIGNED

Volcanoes: eruptive style, pre-eruptive evolution and risk

Total Cost €

EC-Contrib. €

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.

numerical clear doi 1 isotopic data zircons 1016 inherited last age ascension chemistry rocks magmas assimilated obtain subduction deposits patchy mapping herd structure rock mineral storage effusive sub explosive plate active 1007 suitable barclay style volcanoes erupted nature aerial cf texture million magmatic hazards relationship 75 cargoes plumbing experimental mitigate dissolved 014 magma references permit et gt pb context place eruption eruptions event risks constrained periodicity chemgeo shock mixing 2016 crystal ages composition predict suffer crystals thermal description chamberlain s00445 bea jvolgeores relation al 016 02 compositions island constraints few montero longer 006 survive 04 preece events zircon natural 2013 volcanic zoning eruptive geochemical understand identification revealed gertisser prior

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 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.	UK (NORWICH)	coordinator	195˙454.00

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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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