Sub-solidus Oligocene zircon formation in garnet peridotite during fast decompression and fluid infiltration (Duria, Central Alps)
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Hermann, Joerg
Rubatto, Daniela
Trommsdorff, Volkmar
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Springer
Abstract
A garnet peridotite lens from Monte Duria (Adula nappe, Central Alps, Northern Italy) contains porphyroblastic garnet and pargasitic amphibole and reached peak metamorphic conditions of ∼830°C, ∼2.8 GPa. A first stage of near isothermal decompression
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Mineralogy and Petrology
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2037-12-31
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