Related content

THERIA_G: a software program to numerically model prograde garnet growth

By Gaidies F.   Capitani C.   Abart R.  

Contributions to Mineralogy and Petrology, Vol. 155, Iss. 5, 2008-05 ,pp. : 657-671

Springer Publishing Company

Access to resources Recommend Favorite

Hydroxyl in clinopyroxene and titanite in a UHP diamond-free garnet-clinopyroxene rock from the Kokchetav Massif, northern Kazakhstan

By    

International Geology Review, Vol. 56, Iss. 2, 2014-01 ,pp. : 133-149

Taylor & Francis Ltd

Access to resources Recommend Favorite

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

Access to resources Recommend Favorite

Reply to comments on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies: implications for deep subduction zone processes”

By Spandler Carl   Hermann Jörg   Arculus Richard   Mavrogenes John  

Contributions to Mineralogy and Petrology, Vol. 148, Iss. 4, 2004-12 ,pp. : 506-509

Springer Publishing Company

Access to resources Recommend Favorite

Hydrogen partitioning between melt, clinopyroxene, and garnet at 3 GPa in a hydrous MORB with 6 wt.% H 2 O

By Aubaud Cyril  

Contributions to Mineralogy and Petrology, Vol. 156, Iss. 5, 2008-11 ,pp. : 607-625

Springer Publishing Company

Access to resources Recommend Favorite