By M. L. Crawford, L. S. Hollister (auth.), John V. Walther, Bernard J. Wood (eds.)
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Touret, J. S. L. Crawford, 6, 182-208. , and Dietvorst, P. (1983), Fluid inclusions in high-grade anatectic metamorphites. 1. Geol. Soc. London 140, 635-649. F. (1949) Structural petrology of planes of liquid inclusions. 1. Geol. 57, 331-356. R. (1981) l3C1I2C exchange between calcite and graphite: A possible thermometer in Grenville marbles. Geochim. Cosmochim. Acta 45, 411-419. Vidale, R. (1983) Pore solution compositions in a pelitic system at high temperatures, pressures and salinities. Amer.
One isochore (a) corresponds to small, rare, and texturally the earliest formed dense inclusions, and the other two «b), CO 2 + H 20) and «c), CO2 only) to abundant late-formed low-density inclusions. At some stage during uplift, the rocks had to have crossed all the isochores; if the uplift path went outside the shaded region, the densest inclusions probably would have decrepitated or expanded as a result of excess internal pressures greater than 2 kb. 0 ~_ a.. 4 2 400 600 T,oC 800 Fig. 8. Three representative isochores for samples from an uplifted regional meta- morphic terrane.
120, 584-593. , and Morteani, G. (1980) Microthermometrical and chemical studies of fluid inclusions in minerals from Alpine veins from the penninic rocks of the central and western Tauern window (Austria/Italy). Lithos 13, 61-77. Mercolli, I. (1979) Le inclusionifluide nei noduli di quarzo dei marmi dolomitici della regione del Campo lungo (Tieino). Eid. Techn. Hochschule, Zurich. F. (1966) Nitrogen in metamorphic rocks. Geochem. Internat. 3, 752-758. Mullis, J . (1975) Growth conditions of quartz crystals from Val d'Illiez (Valais, Switzerland).