EGU General Assembly 2008
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  Information - GMPV31 Advances in stable isotope geochemistry applied to magmatic and metamorphic systems (co-listed in IG)

Event Information
Stable isotope variations in geological materials may occur both at the meso and micro-scale as a result of equilibrium and/or kinetic reactions. The interpretation of light stable isotope (H, Li, B, C, N, O, S, and Cl isotope) heterogeneity is therefore a key to understand the magmatic and metamorphic processes occurring in crustal and mantle domains. The session focuses to the mechanisms producing isotopic variations, and to their meaning in the geological framework. We therefore welcome insights provided by the re-interpretation of data from classical measurements and by stable isotope data obtained by novel analytical techniques

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The information contained hereafter has been compiled and uploaded by the Session Organizers via the "Organizer Session Form". The Session Organizers have therefore the sole responsibility that this information is true and accurate at the date of publication, and the conference organizer cannot accept any legal responsibility for any errors or omissions that may be made, and he makes no warranty, expressed or implied, with regard to the material published.



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