High fO2 During Sillimanite Zone Metamorphism of Part of the Barrovian Type Locality, Glen Clova, Scotland-Reference-Cited by-同舟云学术

High fO2 During Sillimanite Zone Metamorphism of Part of the Barrovian Type Locality, Glen Clova, Scotland

Published:2001-07 Issue:7 Volume:42 Page:1301-1320
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

AGUE JAY J.,BAXTER ETHAN F.,ECKERT JAMES O.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/42/7/1301/13136079/421301.PDF

Reference57 articles.

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3. Ague, J. J. & Rye, D. M. (1999). Simple models of CO2 release from metacarbonates with implications for interpretation of directions and magnitudes of fluid flow in the deep crust. Journal of Petrology40, 1443–1462.

4. Andersen, D. J. & Lindsley, D. H. (1988). Internally consistent solution models for the Fe–Mg–Mn–Ti oxides: Fe–Ti oxides. American Mineralogist73, 714–726.

5. Baxter, E. F. & DePaolo, D. J. (2000). Field measurement of slow metamorphic reaction rates at temperatures of 500° to 600°C. Science288, 1411–1414.

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