By Dennis A. Carswell, Roberto Compagnoli
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Additional resources for Ultrahigh pressure metamorphism: university textbook
Mineral. Petrogr. , 72:347–363. G. H. (1988): Ge0-calc: Software for calculation and display of pressure-temperature-composition phase diagrams using an IBM or compatible personal computer. Comp. , 14:279–289. , Compagnoni, R. & Rubbo, M. (2001): The ultra-high pressure coronitic and pseudomorphous reactions in a metagranodiorite from the Brossasco-Isasca Unit, Dora-Maira Massif, western Italian Alps: a petrographic study and equilibrium thermodynamic modelling. J. Metamorph. , 19:33–43. , Hirajima, T.
Higher-variance assemblages lacking talc, kyanite, phlogopite I or even garnet I are even more common. Relic coesite, or polycrystalline quartz pseudomorphous after coesite, are present as inclusions in dravite and garnet I2 (mantle of high pressure garnet; Fig. 12). Garnet I2 has also rare inclusions of all other minerals of the UHP stage. 38) + coesite + Mn-epidote + aegirine-augite (Jd26–36Aeg42–51Aug13–24) + hematite + 42 R. Compagnoni & F. Rolfo rutile r apatite r dravite r manganoan dolomite and calcite after former aragonite.
UHPM units in the Western Alps 33 Fig. 9. Petrogenetic grid showing the P–T–t path recorded in the UHP rocks of the Brossasco-Isasca Unit, modified from Compagnoni et al. (1995). Peak metamorphic conditions of the quartz eclogite and blueschist facies units overlying and underlying the BIU, respectively, are also shown. Prograde path mainly follows Schertl et al. (1991) with supplementary data from a newly found relict Cl-bearing hornblende included in eclogite garnet and from a pre-Alpine almandine garnet in paraschist.