Mineralogical Evidence for Fluid–Rock Interaction Accompanying Prograde Contact Metamorphism of Siliceous Dolomites: Alta Stock Aureole, Utah, USA-Reference-Cited by-同舟云学术

Mineralogical Evidence for Fluid–Rock Interaction Accompanying Prograde Contact Metamorphism of Siliceous Dolomites: Alta Stock Aureole, Utah, USA

Published:2000-06-01 Issue:6 Volume:41 Page:739-757
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

COOK STEPHEN J.,BOWMAN JOHN R.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/41/6/739/21429914/egd036.pdf

Reference32 articles.

1. Baumgartner, L. P. & Ferry, J. M. (1991). A model for coupled fluid-flow and mixed-volatile mineral reactions with applications to regional metamorphism. Contributions to Mineralogy and Petrology106, 273–285.

2. Baker, A. A., Calkins, F. C., Crittenden, M. D. & Bromfield, C. S. (1966). Geologic map of the Brighton quadrangle, Utah. US Geological Survey Map GQ-535, 7′5′′.

3. Bowers, T. S. & Helgeson, H. C. (1983). Calculation of the thermodynamic and geochemical consequences of nonideal mixing in the system H2O–CO2–NaCl on phase relations in geologic systems: equation of state for H2O–CO2–NaCl fluids at high pressures and temperatures. Geochimica et Cosmochimica Acta47, 1247–1275.

4. Bowman, J. R., Willett, S. D. & Cook, S. J. (1994). Oxygen isotopic transport and exchange during fluid flow: one-dimensional models and applications. American Journal of Science294, 1–55.

5. Cartwright, I. & Buick, I. S. (1996). Determining the direction of contact metamorphic fluid flow: an assessment of mineralogical and stable isotope criteria. Journal of Metamorphic Geology14, 289–305.

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