Reply to: Comments on the paper "Multiple fluid migration events in the Sopron Gneisses during the Alpine high-pressure metamorphism, as recorded by bulk-rock and mineral chemistry and fluid inclusions" by Kálmán Török

By Török Kálmán  

Neues Jahrbuch für Mineralogie - Abhandlungen: Journal of Mineralogy and Geochemistry, Vol. 178, Iss. 1, 2002-12 ,pp. : 99-106

E. Schweizerbart'sche Verlagsbuchhandlung

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Multiple fluid migration events in the Sopron Gneisses during the Alpine high-pressure metamorphism, as recorded by bulk-rock and mineral chemistry and fluid inclusions

By Török Kálmán  

Neues Jahrbuch für Mineralogie - Abhandlungen: Journal of Mineralogy and Geochemistry, Vol. 177, Iss. 1, 2001-12 ,pp. : 1-36

E. Schweizerbart'sche Verlagsbuchhandlung

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Re-equilibration of a high-pressure metamorphic fluid: evidence from tourmaline-, apatite- and quartz-hosted fluid inclusions in an Eoalpine eclogite from the Eastern Alps

By Krenn Kurt   Konzett Jürgen   Hoinkes Georg  

European Journal of Mineralogy, Vol. 26, Iss. 2, 2014-03 ,pp. : 231-244

E. Schweizerbart'sche Verlagsbuchhandlung

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Ultra-high-pressure metamorphism in felsic rocks: the garnet-phengite gneisses and quarzites from the Lanterman Range, Antarctica

By Palmeri Rosaria   Ghiribelli Barbara   Talarico Franco   Ricci Carlo Alberto  

European Journal of Mineralogy, Vol. 15, Iss. 3, 2003-06 ,pp. : 513-525

E. Schweizerbart'sche Verlagsbuchhandlung

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Evidence for diamond-grade ultra-high pressure metamorphism and fluid interaction in the Svartberget Fe–Ti garnet peridotite–websterite body, Western Gneiss Region, Norway

By Vrijmoed J. C.   Van Roermund H. L. M.   Davies G. R.  

Mineralogy and Petrology, Vol. 88, Iss. 1-2, 2006-09 ,pp. : 381-405

Springer Publishing Company

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