Goldschmidt Session – 6g Pathways and Processes in Differentiation of Arc Magmatic Systems

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From: colin.macpherson@xxxxxxxxxxxx

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** Goldschmidt Session â?? 6g Pathways and Processes in Differentiation of
Arc Magmatic Systems **



## Convenors â?? Colin Macpherson, Christy Till, Lucy McGee ##



Subduction zones host some of the planetâ??s most important magmatic systems,
provide mineral and geothermal resources, and valuable, fertile land yet
they are also responsible for devastating natural hazards. Furthermore,
such systems are also sites of refinement, and potentially growth, of
continental crust. Therefore, understanding the sources of magma, their
pathways through the crust, and processes of differentiation are of major
scientific and social importance. Achieving this understanding relies on
knowledge of many factors including: the age, composition, and prior
tectonic history of the overriding plate; the composition of primary magma
arriving into the arc lithosphere; the rheologic and thermal profile of arc
lithosphere; the evolving stress field associated with the convergent
margin; the role of reactive pathways exploited by melts; and the longevity
of the magmatic system(s). Each of these factors, which may also vary along
strike, influences the pressure, temperature, oxygen fugacity, vapour
saturation, and crustal contamination that affect particular magma batches
emplaced into or through the arc lithosphere. Ultimately, these processes
potentially impact, for better or worse, the communities around them.

We invite submissions that explore the feedbacks and interactions between
intrinsic and extrinsic properties of subduction zone magmas to understand
their origin, pathways and differentiation. Petrological, geochemical, and
geochronological studies of natural systems, and experimental and numerical
simulations of magmatic systems are welcomed. We also encourage
contributions that seek to relate both these approaches to the wider
tectonic, metamorphic, and geophysical structure of convergent margins, and
the societal impact of their volcanism.

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