2006 EGU Spring Meeting: The origin of the slab component in island arcs

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2006 EGU Spring Meeting Session Reminder: 
The origin of the slab component in island arcs
************************************************
From: Timm John <tj@xxxxxxxxxxxxxxx>


Dear newsgroup member   -apologies for multiple postings-,

we would like to remind you of the session "The origin of the slab  
component in island arcs: H2O-rich fluid or melt- who delivers the  
goods?" at the 2006 EGU Meeting ( http://www.cosis.net/members/ 
meetings/programme/view.php?m_id=29&p_id=195 ).
The meeting is being held in Vienna, Austria on April 02 to 07, 2006.

Abstract deadline is January 13

Our solicited speakers to date are Horst Marschall (University of  
Bristol), Taras Gerya (ETH Zuerich) and Marco Scambelluri (Universita  
di Genova).

Best regards,
Thomas Zack and Timm John

The origin of the slab component in island arcs: H2O-rich fluid or  
melt- who delivers the goods? (GMPV5)

There is a consensus in the geoscience community that arc magmatism  
has a distinct chemical signature due to the addition of certain  
trace elements (e.g. Li, B, LILE, LREE) carried by slab-derived  
agents. What has yet to be established are the mechanisms by which  
these elements are transported from sources within the slab into the  
overlying wedge, and how fluids or melts -- or both -- are related to  
this process. Current debate centers on whether melts are the main or  
even sole agent responsible for the mobilization of the required  
amounts of trace elements. Some studies suggest that hydrous fluids  
are sufficiently reactive to scavenge these elements in open systems.  
Also under discussion are the subducted sediments, which are thought  
to be an important trace element source. Confirming or contradicting  
these claims will place first order constraints on the thermal  
structure of subduction zones. In this session we will address these  
issues by bringing together experimental and metamorphic  
petrologists, geochemists, geophysists, and modelers. "

------------------------------------
Thomas Zack
Mineralogisches Institut
Universitaet Heidelberg
INF 236
69120 Heidelberg
Germany
tzack at min.uni-heidelberg.de

Timm John
Institut für Geowissenschaften, Abteilung Mineralogie - Petrologie
Universität Kiel
D-24098 Kiel, Germany
tj at min.uni-kiel.de

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