Garnet growth as a proxy for progressive subduction zone dehydration
Author:
Publisher
Geological Society of America
Subject
Geology
Link
http://pubs.geoscienceworld.org/geology/article-pdf/41/6/643/3544378/643.pdf
Reference33 articles.
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3. Quantifying the tectono-metamorphic evolution of pelitic rocks from a wide range of tectonic settings: Mineral compositions in equilibrium;Caddick;Contributions to Mineralogy and Petrology,2008
4. Preservation of garnet growth zoning and the duration of prograde metamorphism;Caddick;Journal of Petrology,2010
5. The lawsonite paradox: A comparison of field evidence and mineral equilibria modeling;Clarke;Journal of Metamorphic Geology,2006
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