An automated method for the calculation of P-T paths from garnet zoning, with application to metapelitic schist from the Kootenay Arc, British Columbia, Canada-Reference-Cited by-同舟云学术

An automated method for the calculation of P-T paths from garnet zoning, with application to metapelitic schist from the Kootenay Arc, British Columbia, Canada

Published:2013-03-16 Issue:5 Volume:31 Page:525-548
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Meta. Geol.

Author:

Moynihan D. P.¹²,Pattison D. R. M.¹

Affiliation:

1. Department of Geoscience; University of Calgary; Calgary AB T2N 1N4 Canada

2. Yukon Geological Survey; P.O. Box 2703 (K-14) Whitehorse Yukon Y1A 2C6 Canada

Funder

NSERC Discovery

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12032/fullpdf

Reference70 articles.

1. Inclusion patterns in zoned garnets from Mageroy, north Norway;Andersen;Mineralogical Magazine,1984

2. Geochronology and tectonic implications of magmatism and metamorphism, southern Kootenay Arc and neighbouring regions, southeastern British Columbia. Part I: Jurassic to mid-Cretaceous;Archibald;Canadian Journal of Earth Sciences,1983

3. Geochronology and tectonic implications of magmatism and metamorphism, southern Kootenay Arc and neighbouring regions, southeastern British Columbia. Part II: Mid-Cretaceous to Eocene;Archibald;Canadian Journal of Earth Sciences,1984

4. Garnet-quartz intergrowths in graphitic pelites: the role of the fluid phase;Burton;Mineralogical Magazine,1986

5. The computation of chemical equilibrium in complex systems containing non-ideal solutions;de Capitani;Geochimica et Cosmochimica Acta,1987

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