EGU session 'Micro to macroscale advances in volcano-earthquake interactions' (GMPV5.4/NH2.8/TS10.4)

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From: Lauren Schaefer <lauren.n.schaef@xxxxxxxxx>

5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5-5


Dear colleagues,

The 2019 EGU abstract deadline is fast approaching and we'd like to draw
your attention to the following session:

*Micro to macroscale advances in volcano-earthquake interactions (*
*GMPV5.4/NH2.8/TS10.4)*

EGU General Assembly 2019, Vienna | Austria | 7â??12 April 2019
________________________________________________

Volcanoes and earthquakes may be communicating on different scales and in
different ways. Volcanoes may be activated after tectonic earthquakes,
neighbouring volcanoes become simultaneously active, and volcanoes may
activate faults. The interactions may work on spatial distances exceeding
hundreds of kilometres. This session provides a forum to discuss novel
research related to volcano interactions. For example, how is stress
transferred between intrusions and faults? What are the effects of a
seismic wave passing through magma? What are the specific conditions for
these waves to impart damage to volcanic material, and at what point will
the material fail or magma erupt?

The characterisation of earthquake-induced strain to a volcanic edifice, or
changes in the magmatic system, is complicated by the systemâ??s inherent
heterogeneity and behaviour at different spatial and temporal scales. This
session aims to highlight advances in volcano-earthquake interactions from
experimental, geophysical, numerical, analogue, analytical, statistical,
theoretical, remote sensing or fieldwork studies. We welcome insights from
regional-scale tectonic studies to lab-scale bubble experiments, and
everything in between in the hope to develop synergy between researchers
across the spectrum of approaches. This can include, but is not limited to,
contributions on the following topics:

â?¢ Earthquake-triggered eruptions, and vice versa
â?¢ Fault dynamics near volcanoes
â?¢ Mechanisms of earthquake-triggered tensional or shear failures
â?¢ Dynamic experiments (high pressure, high temperature, phase-change,
cyclic, etc.)
â?¢ Velocity changes during volcanic rock deformation and failure
â?¢ Measurements of earthquake-induced rock damage
â?¢ Magma reactions and fragmentation
â?¢ Bubble dynamics
â?¢ Cascading volcano-earthquake hazards
________________________________________________

*Abstracts can be submitted here
<https://meetingorganizer.copernicus.org/EGU2019/session/32726> by January
10, 13:00 CET.*

Looking forward to seeing you in Vienna!
Lauren Schaefer, Jackie Kendrick, and Thomas Walter

==============================================================

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