Fall AGU Union Session: Fluids at Convergent Margins

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From: Alison Shaw <ashaw@xxxxxxxx>
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Dear Colleagues,

Please consider submitting an abstract to the following Union session at this
Fall's AGU meeting (15-19 December). This session will bring together
researchers from a diverse set of backgrounds who study the role of fluids at
convergent margins.

All the best,
Alison Shaw

Please not that the abstract deadline is September 10.

U20: Fluids at Convergent Margins: Synthesis of Observations, Experiments and
Models

Conveners:  Peter van Keken (University of Michigan), Alison Shaw (WHOI,Demian
Saffer (Penn State), Kaj Hoernle (IFM-Geomar)

Invited speakers: Karen Fisher (Brown University), Gray Bebout (Lehigh
University), Ikuko Wada (Pacific Geoscience Centre), Cesar Ranero (Instituto de
Ciencias del Mar)

Water and other fluids play defining roles in subduction zone processes over a
wide range of depths and scales. At shallow levels these processes include
diagenesis and alteration, fault zone stability and seismogenesis, and coupling
of deformation between subducting and overriding plate. Fluids likely play an
important role in controlling shallow seismic events at the plate interface.
Deeper in the subduction zone fluids control dehydration and metamorphic
reactions, magma formation and migration, rheology and dynamics of the mantle
wedge, and generation of intermediate-depth seismicity. Characterizing the role
of fluids and volatiles has been a key component of international and
collaborative subduction zone research projects, that include the Seismogenic
Zone Experiment (SEIZE) and Subduction Factory (Subfac) initiatives of the NSF
MARGINS program, the Japanese IFREE program, the German SFB574 collaborative
research center and the Russian-German KALMAR collaborative project, with focus
sites at Nankai, Central America, Central Chile, Kamchatka, and
Izu-Bonin-Marianas. These efforts have led to unprecedented advances in our
understanding of the role of fluids in the formation and maintenance of the
seismogenic zone and the connection between the inputs and outputs of the
subduction factory. In-situ observations of fluids in subduction zones remains
difficult, but the additional use of indirect observations coupled with
integrated experimental and theoretical work has allowed for significant
progress. This session will further the synthesis of observational, theoretical
and experimental research on the role of fluids in subduction zones. This
session is intended to bring together researchers from various fields with
interests that cut across traditional discipline boundaries. We invite
contributions from a wide range of disciplines including geodesy, ocean
drilling, hydrology, volcanology, seismology, petrology, geodynamics, and
geochemistry.

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