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  Information - VGP8 The role of accessory minerals in rocks: petrogenetic indicators of metamorphic and igneous processes

Event Information
Accessory minerals in most metamorphic and igneous rocks nominally include apatite, monazite, xenotime, zircon, titanite, most sulphides and oxides, as well as a wide range of more exotic varieties such as REE-, Th-, and U-bearing silicates. In many cases, careful chemical analysis and petrographic characterization of an accessory mineral can be instrumental in determining the age of a rock, oxygen and sulphur fugacities, or whether metasomatic processes may have occurred, and if so, the approximate composition of the fluids responsible for the metasomatism as well as the P-T conditions under which the metasomatism occurred. In addition, experimental investigations provide important independent constraints on the stability fields of these minerals as well as their relationship to the major rock-forming silicate minerals.

The goal of this session is to bring together mineralogists, petrologists, and geochemists to discuss the most recent advances in mineralogical/petrological geochemical and experimental research regarding accessory minerals with respect to what they can tell us about petrogenetic processes in both metamorphic and igneous environments.

Preliminary List of Solicited Speakers
Reto Giere
Fredrich Finger
Christian Chopin
Andrew Putnis

Co-Sponsorship

General Statement
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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