Abstract: Post-magmatic structural evolution of the Troodos Ophiolite Pillow Lavas revealed by microthermometry within vein precipitates, with application to Alpine-Mediterranean supra-subduction zone settings (2017 AGU Fall Meeting)

Post-magmatic structural evolution of the Troodos Ophiolite Pillow Lavas revealed by microthermometry within vein precipitates, with application to Alpine-Mediterranean supra-subduction zone settings

Walter Kurz¹, Dennis Quandt², Peter Micheuz² and Kurt Krenn³, (1)University of Graz, Department of Earth Sciences, NAWI Graz Geocenter, Graz, Austria, (2)University of Graz, Institute of Earth Sciences, Graz, Austria, (3)University of Graz, Graz, Austria

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