Sapphirine as a Breakdown Product of Garnet in a Variscan UHP/HT Peridotite from the Vosges Mountains (France) – An Indication of Near-Isothermal Decompression
Author:
Affiliation:
1. Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234-236, D-69120 Heidelberg, Germany
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/petrology/article-pdf/59/11/2221/27239425/egy096.pdf
Reference94 articles.
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3. Metamorphic evolution of ultrahigh-pressure garnet peridotites from the Variscan Vosges Mts. (France);Altherr;Chemical Geology,1996
4. High-potassium, calc-alkaline I-type plutonism in the European Variscides: northern Vosges (France) and northern Schwarzwald (Germany);Altherr;Lithos,2000
5. Evidence from ultra-high-pressure marbles for recycling of sediments into the mantle;Becker;Nature,1992
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