H 2 O in omphacite of quartz and coesite eclogite from Erzgebirge and Fichtelgebirge, Germany
Author:
Affiliation:
1. Geozentrum Nordbayern University Erlangen‐Nürnberg Erlangen Germany
Funder
Deutsche Forschungsgemeinschaft
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12642
Reference61 articles.
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2. Water in the Earth's mantle: The role of nominally anhydrous minerals;Bell D. R.;Science,1992
3. The distribution of hydroxyl in garnets from the subcontinental mantle of southern Africa;Bell D. R.;Contributions to Mineralogy and Petrology,1992
4. An experimental investigation of hydroxyl solubility in jadeite and Na‐rich clinopyroxenes;Bromiley G. D.;Contributions to Mineralogy and Petrology,2004
5. H2O abundance in depleted to moderately enriched mid‐ocean ridge magmas; part I: Incompatible behaviour, implications for mantle storage, and origin of regional variations;Danyushevski L. V.;Journal of Petrology,2000
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