Mass transfer and fluid evolution in late-metamorphic veins, Rhenish Massif (Germany): insight from alteration geochemistry and fluid-mineral equilibria modeling-Reference-Cited by-同舟云学术

Mass transfer and fluid evolution in late-metamorphic veins, Rhenish Massif (Germany): insight from alteration geochemistry and fluid-mineral equilibria modeling

Published:2016-01-27 Issue:4 Volume:110 Page:515-545
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Miner Petrol

Author:

Marsala Achille,Wagner Thomas

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00710-016-0424-8.pdf

Reference103 articles.

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2. Ague JJ (1994b) Mass transfer during Barrovian metamorphism of pelites, south-central Connecticut; II, Channelized fluid flow and the growth of staurolite and kyanite. Am J Sci 294:1061–1134

3. Ague JJ (1997) Compositional variations in metamorphosed sediments of the Littleton Formation, New Hampshire; discussion. Am J Sci 297:440–449

4. Ague JJ (2003) Fluid flow in the deep crust. In: Heinrich DH, Karl KT (eds) Treatise on geochemistry. Pergamon, Oxford, pp 195–228

5. Ague JJ (2011) Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism. Am Mineral 96:333–352

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