PhD position: ISTeP, Paris

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From: Helene BALCONE BOISSARD <
helene.balcone_boissard@xxxxxxxxxxxxxxxxxxxxxx>


*Characterization of the unrest dynamics of volcanoes and eruption
forecasting*

*Keywords*

Neapolitan Volcanoes, Minerals Microanalysis, Diffusion Chronometry,
experimental petrology



*Summary of thesis project*

Active volcanoes represent a source of natural hazards quite diffuse on
Earth. In densely populated areas, their presence poses high risks,
affecting both land use management and urban development. This issue
stimulates a continuously growing interest in unravelling the natural
processes that trigger eruptions and control eruptive dynamics. The ability
to monitor active volcanoes using seismic signals, ground deformation, gas
flux and composition, and any other ground- and satellite-based
observations, as well as the understanding of the behaviour of magma
reservoirs that feed eruptions have evolved enormously in recent years.
However, the dynamics of complex plumbing systems that feed eruptions,
specifically those with explosive character, are difficult to relate
straightforwardly to the monitoring signals. This makes the management of
unrest phases, as well as the forecasting of explosive eruptions,
particularly difficult challenging.

Understanding whether the unrest phase of an active volcano will or will
not end with an eruption is perhaps the main challenge volcanologists and
civil protection operators are facing, especially in those active volcanic
areas where unrest lasts for decades without leading to an eruption. *Among
these areas we may count the Neapolitan area, with the Campi Flegrei and
Ischia volcanic fields and Mount Somma-Vesuvio.* *The aim is to unravel the
precursor phenomena of volcanic eruptions in the case of the neapolitan
volcanoes.*



The major goal of the PhD project is to study in detail a volcanic eruption
that occurred in historical time in the Neapolitan area (on Ischia island
and on Mt. Somma-Vesuvio). Here the Arso eruption (Ischia Island) and the
1631 and 1944 A.D. eruptions (Mt. Vesuvius) will be investigated. These
eruptions are characterized by different eruptive styles (they are both
effusive and explosive types of eruptions) and magma chamber dynamics and
conduit processes (open/closed). We intend to study the features of the
plumbing systems feeding these eruptions in terms of pre-eruptive magmatic
processes and eruptive dynamics, and constrain their timescales.
Experimental petrology describing the magma chamber dynamic or ascent in
the conduit can be a path followed by the subject as a complement to
petrogeochemical research on natural products.



*Context of thesis project*

The PhD project is proposed in the framework of the SMEEGOL project,
â??historical
Sources, Minerals microanalysis, Experimental pEtrology and numerical
modellinG to unravel the precursor phenomena Of voLcanic eruptions: the
case of the Neapolitan volcanoesâ??.



*Expected results*

The expected results are a high-level formation in petrology and
volcanology in close collaboration between Paris and Napoli. The student
will discuss key results on pre-eruptive magma dynamics indicator of
precursors of volcanic eruption to define an early-warning clock.



*Profile and skills required*

We are seeking an autonomous and hard-worker student but able to work
easily with different people between France and Italy. Former experiences
in magmatic petrology and geochemistry will be an advantage, as well as
skills in point analyses (SEM, EPMA, SIMS, LA-ICP-MS).



Contact : Hélène Balcone-Boissard, ISTeP, Paris;
helene.balcone_boissard@xxxxxxxxxxxxxxxxxxxxxx


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End of Volcano Digest - 6 Apr 2023 to 7 Apr 2023 (#2023-39)
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