Oxy-substitution and dehydrogenation in mantle-derived amphibole megacrysts
- 1 November 1999
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 63 (21) , 3635-3651
- https://doi.org/10.1016/s0016-7037(99)00162-3
Abstract
No abstract availableKeywords
This publication has 61 references indexed in Scilit:
- Ferric iron in peridotites and mantle oxidation statesPublished by Elsevier ,2002
- The generation of oxidized CO2-bearing basaltic melts from reduced CH4-bearing upper mantle sourcesGeochimica et Cosmochimica Acta, 1994
- The effects of pressure and temperature on the partitioning of Ti, Sr and REE between amphibole, clinopyroxene and basanitic meltsChemical Geology, 1994
- Carbon–fluid equilibria and the oxidation state of the upper mantleNature, 1991
- The redox states of basic and silicic magmas: a reflection of their source regions?Contributions to Mineralogy and Petrology, 1991
- Intrinsic oxygen fugacity measurements: techniques and results for spinels from upper mantle peridotites and megacryst assemblagesGeochimica et Cosmochimica Acta, 1981
- Late Cenozoic Alkalic Basaltic Magmas in the Western Colorado Plateaus and the Basin and Range Transition Zone, U.S.A., and Their Bearing on Mantle DynamicsGSA Bulletin, 1974
- High pressure megacrysts in alkaline lavas from northeastern New South WalesAmerican Journal of Science, 1970
- Kaersutite-peridotite inclusions and kindred megacrysts in basanitic lavas, Grand Canyon, ArizonaContributions to Mineralogy and Petrology, 1970
- The Kaersutites and Oxykaersutites from Alkalic Rocks of Japan and Surrounding AreasJournal of Petrology, 1963