Hermann, JoergRubatto, DanielaTrommsdorff, Volkmar2015-12-070930-0708http://hdl.handle.net/1885/19813A 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 decompressionSub-solidus Oligocene zircon formation in garnet peridotite during fast decompression and fluid infiltration (Duria, Central Alps)200610.1007/s00710-006-0155-32015-12-07