Oxygen isotope exchange and disequilibrium between calcite and tremolite in the absence and presence of an experimental C–O–H fluid

By Zheng Y.-F.   Satir M.   Metz P.  

Contributions to Mineralogy and Petrology, Vol. 146, Iss. 6, 2004-02 ,pp. : 683-695

Springer Publishing Company

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Influence of temperature, composition, silica activity and oxygen fugacity on the H 2 O storage capacity of olivine at 8 GPa

By Withers Anthony  

Contributions to Mineralogy and Petrology, Vol. 156, Iss. 5, 2008-11 ,pp. : 595-605

Springer Publishing Company

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Genesis and evolution of subduction-zone andesites: evidence from melt inclusions

By Zhu Ming-Shuai   Miao Lai-Cheng   Yang Shun-Hu  

International Geology Review, Vol. 55, Iss. 10, 2013-07 ,pp. : 1179-1190

Taylor & Francis Ltd

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Origin of eclogite and garnet pyroxenite from the Moldanubian Zone of the Bohemian Massif, Czech Republic and its implication to other mafic layers embedded in orogenic peridotites

By Obata M.   Hirajima T.   Svojtka M.  

Mineralogy and Petrology, Vol. 88, Iss. 1-2, 2006-09 ,pp. : 321-340

Springer Publishing Company

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Decoupling of fluid and trace element release in subducting slab? Comment on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes” by C. Spandler et al. (Contrib Mineral Petrol 146:205–222, 2003)

By Liebscher Axel  

Contributions to Mineralogy and Petrology, Vol. 148, Iss. 4, 2004-12 ,pp. : 502-505

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