Invitation to IAVCEI 2013 Session 3.3a: "Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources"
From: Adelina Geyer Traver <ageyertraver@xxxxxxxxx>
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Dear Colleague,
We would like to encourage you to contribute with a presentation to the session on "Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources" (3.3a) at the IAVCEI 2013 Scientific Assembly , 20-24 July 2013 (http://www.iavcei2013.com/) .
We would like to encourage you to contribute with a presentation to the session on "Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources" (3.3a) at the IAVCEI 2013 Scientific Assembly , 20-24 July 2013 (http://www.iavcei2013.com/) .
Deadline for receipt of abstracts is 31 January 2013.
The conveners are Adelina Geyer (CSIC, Spain), Valerio Acocella (Roma Tre University, Italy) and Nobuo Geshi (Geological Survey of Japan, Japan)
A description of the session is provided below.
Please pass this information on to colleagues and students working in this field.
We apologize for any multiple posting and look forward to meet you in Kagoshima.
Thank you.
Kind regards,
Adelina Geyer
Valerio Acocella
Nobuo Geshi
Calderas: Context, formation, evolution, structure, unrest, products, hazard, resources
Calderas
are the most distinctive and dramatic collapse feature of volcanoes.
This session aims at providing the state of the art on the main
processes accompanying the development of calderas, including their
regional tectonic and magmatic context, the conditions for their
formation and evolution, their structure and effect on eruptive
activity, the role of magma and/or hydrothermal systems on the
frequently observed unrest episodes, the impact of unrest and eruptions
on hazard and the role of calderas as source for geothermal and ore
exploitation.
Ultimate questions,
which we will address, include the following. Which are the conditions
leading to caldera unrest? How does unrest evolve into an eruption? How
caldera formation and structure may affect volcanic activity? Is there
any common behaviour or feature in the development and structure of
calderas?
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Dr. Adelina Geyer Traver
Institute of Earth Sciences "Jaume Almera" (CSIC)
C/Lluis Solé i Sabaris s/n
08028 Barcelona
Spain
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