IAVCEI General Assembly 2008: Chambers and Conduits 1 (1-k)

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From: Raymond Cas <Ray.Cas@xxxxxxxxxxxxxxxxx>
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Dear Colleagues,

We invite everyone who is interested to submit abstracts for the
following symposium at the 2008 IAVCEI General Assembly in Reykjavik,
Iceland, 18-22 August, 2008.  The abstract submission deadline is 1
April 2008.  Further information about the conference and abstract
submission process can be
found at http://www.iavcei2008.hi.is/page/I08-intro. We look forward to
a very stimulating, interdisciplinary symposium on this intriguing topic.

1-k CHAMBERS AND CONDUITS I: GEOPHYSICAL, GEOCHEMICAL AND GEOLOGICAL
OBSERVATIONS

Conveners:
Ray Cas, School of Geosciences, Monash University, ray.cas@xxxxxxxxxxxxxxxxx
Hugh Tuffen,Department of Environmental Science, Lancaster University,
h.tuffen@xxxxxxxxxxxxxxx
Freysteinn Sigmundsson, Nordic Volcanological Center, Institute of Earth
Sciences, University of Iceland, fs@xxxxx

This session is dedicated to understanding the characteristics and
dynamics of magma chambers, the magma conduits to the Earth's surface
and volcanic vents, based on geophysical, geochemical and geological
data and observations.

This session will focus on:
- Imaging magma chambers and conduits using geophysical and remote
sensing data sets and understanding their behaviour.
- Understanding the time-scales of magma chamber formation, evolution,
longevity, recharge, and closed system versus open system state.
- Using geochemical approaches to constrain the timescale and mechanism
of degassing and flow in shallow conduits
- Understanding the role of geochemical processes in triggering
eruptions (e.g. differentiation, fractionation, volatile behaviour,
magma mixing)
- Using geological studies of ancient magma chambers, magma conduits and
vents to understand how magma chambers form and evolve, the processes of
magma conduit formation and propagation, and the processes of vent
formation and evolution.

Case studies of all magma system types from ultrabasic komatiites and
kimberlites, to basaltic, intermediate and silicic magma systems, and
involving non-eruptive to effusive lava forming eruptions to explosive
eruption systems, and a spectrum of volcano types will be welcome.
Approaches that employ a combination of geophysical, geochemical and
geological approaches are particularly encouraged.

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