Quantitative P-T paths from zoned minerals: Theory and tectonic applications

Author:

Spear Frank S.,Selverstone Jane

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference34 articles.

1. Althaus E, Karotke E, Nitsch KH, Winkler HGF (1970) An experimental reexamination of the upper stability limit of muscovite plus quartz. Neues Jahrb Mineral Monatsh: 325?336

2. Anderson DE, Olimpio JC (1977) Progressive homogenization of metamorphic garnets, South Morar, Scotland: evidence for volume diffusion. Can Mineral 15:205?216

3. Burnham CW, Holloway JR, Davis NF (1969) Thermodynamic properties of water to 1000° C and 10,000 bars. Geol Soc Amer spec pap 132, pp 96

4. Crawford ML, Mark LE (1982) Evidence from metamorphic rocks for overthrusting, Pennsylvania Piedmont, USA. Can Mineral 20:330?347

5. Dietvorst EJL (1982) Retrograde garnet zoning at low water pressure in metapelitic rocks from Kemio, SW Finland. Contrib Mineral Petrol 79:37?45

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