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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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Restricted until

2037-12-31