Fluid production rate during the regional metamorphism of a pelitic schist
Author:
Funder
Division of Earth Sciences
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00410-018-1523-9/fulltext.html
Reference93 articles.
1. Aagaard P, Helgeson HC (1982) Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions. 1. Theoretical solutions. Am J Sci 282(3):237–285
2. Ague JJ (1991) Evidence for major mass transfer and volume strain during regional metamorphism of pelites. Geology 19(8):855–858 https://doi.org/10.1130/0091-7613(1991)019%3C0855:EFMMTA%3E2.3.CO;2
3. Ague JJ (2003) Fluid infiltration and transport of major, minor, and trace elements during regional metamorphism of carbonate rocks, Wepawaug Schist, Connecticut, USA. Am J Sci 303(9):753–816. https://doi.org/10.2475/ajs.303.9.753
4. Ague JJ (2011) Extreme channelization of fluid and the problem of element mobility during Barrovian metamorphism. Am Miner 96(2–3):333–352. https://doi.org/10.2138/am.2011.3582
5. Ague JJ (2014) 4.6 - Fluid Flow in the Deep Crust A2 - Holland, Heinrich D. In: Turekian KK (ed) Treatise on Geochemistry (Second Edition). vol. Elsevier, Oxford, pp 203–247
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