Internal and external fluid sources for eclogite-facies veins in the Monviso Meta-ophiolite, Western Alps: Implications for fluid flow in subduction zones
To contribute to our understanding of the mechanisms and pathways of fluid movement through deeply subducted crust, we investigate high-pressure veins cutting eclogite-facies (~2·0 GPa and ~600°C) metagabbros of the Monviso Ophiolite, Italian Western Al
|Collections||ANU Research Publications|
|Source:||Journal of Petrology|
|01_Spandler_Internal_and_external_fluid_2011.pdf||2.27 MB||Adobe PDF||Request a copy|
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