Quantitative P-T paths from zoned minerals: Theory and tectonic applications-Reference-Cited by-同舟云学术

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

Published:1983-09 Issue:3-4 Volume:83 Page:348-357
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Spear Frank S.,Selverstone Jane

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00371203.pdf

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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