Call for Abstract - EGU 2020, Vienna 3-8 May - GMPV8.1-Rates, timescales and mechanisms of plutonic and volcanic processes: from mantle source to emplacement or eruption

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From: Fabio Arzilli <arzilli.fabio@xxxxxxxxx>

Dear Colleagues,


We would like to draw your attention to the session GMPV8.1 â??Rates,
timescales and mechanisms of plutonic and volcanic processes: from mantle
source to emplacement or eruptionâ?? at the next European Geosciences Union
(EGU) General Assembly in Vienna (Austria), 3-8 May 2020. The session is
part of EGU and AGU joint session, which is hosted at each EGU and AGU
meeting, sponsored by respectively EGUâ??s GMPV and AGUâ??s VGP. The detailed
description of the session is below. The abstract submission deadline is
January 15.

To submit your abstract, go to the session GMPV8.1 at:
https://meetingorganizer.copernicus.org/EGU2020/session/35185



*Session details*

GMPV8 â?? Advances in igneous petrology

Session: GMPV8.1 â?? Rates, timescales and mechanisms of plutonic and
volcanic processes: from mantle source to emplacement or eruption

Convener: Fabio Arzilli (University of Manchester, UK), Co-conveners:
Maurizio Petrelli (University of Perugia, Italy), Madison Myers (Montana
State University, U.S.), Georg Zellmer (Massey University, New Zealand)



*Session description*

Magmatic and volcanic systems involve a range of dynamic processes that
govern magma generation, ascent, emplacement, and eruption. The timescales
of these processes are of paramount importance to understanding the
evolution of magmatic reservoirs and mush zones during crystallisation,
assimilation, mixing, and volatile exsolution. Depending on the ascent
timescale, these processes may operate far from compositional and textural
equilibrium, induced by rapidly changing environmental parameters (e.g., P,
T, fO2).


Rates and mechanisms of crustal emplacement or eruption, are also crucial
in characterising volcanic hazards. We welcome analytical, numerical,
experimental, geophysical, and field-based studies addressing rates and
timescales of volcanic and plutonic processes. These may include radiogenic
isotope dating, mineral geospeedometry, in situ X-ray microtomography
experiments, crystal size distribution analysis, and fluid dynamics. Also,
we welcome interdisciplinary studies probing the mechanisms and timescales
of volcanic phenomena. We finally encourage studies highlighting the role
of time in characterising volcanic hazards and how improved knowledge adds
societal support for fast response to rapidly evolving geological processes.


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