OH-defects in multiple-doped orthoenstatite at 4–8 GPa: filling the gap between pure and natural systems
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/article/10.1007/s00410-015-1133-8/fulltext.html
Reference40 articles.
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2. Bell DR, Ihinger PD, Rossman GR (1995) Quantitative analysis of trace OH in garnet and pyroxenes. Am Mineral 80:465–474
3. Bell DR, Rossman GR, Moore RO (2004) Abundance and partitioning of OH in a high-pressure magmatic system: megacrysts from the monastery kimberlite, South Africa. J Petrol 45:1539–1564
4. Frey FA, Prinz M (1978) Ultramafic inclusions from San-Carlos, Arizona—petrologic and geochemical data bearing on their petrogenesis. Earth Planet Sci Lett 38:129–176
5. Grant K, Ingrin J, Lorand JP, Dumas P (2007) Water partitioning between mantle minerals from peridotite xenoliths. Contrib Mineral Petrol 154:15–34
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