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Faryad, Shah Wali, Nahodilová, Radmila, Dolejš, David (2010) Incipient eclogite facies metamorphism in the Moldanubian granulites revealed by mineral inclusions in garnet. Lithos, 114 (1) 54-69 doi:10.1016/j.lithos.2009.07.014

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Reference TypeJournal (article/letter/editorial)
TitleIncipient eclogite facies metamorphism in the Moldanubian granulites revealed by mineral inclusions in garnet
JournalLithos
AuthorsFaryad, Shah WaliAuthor
Nahodilová, RadmilaAuthor
Dolejš, DavidAuthor
Year2010 (January)Volume114
Issue1
PublisherElsevier BV
DOIdoi:10.1016/j.lithos.2009.07.014Search in ResearchGate
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Mindat Ref. ID272102Long-form Identifiermindat:1:5:272102:0
GUID0
Full ReferenceFaryad, Shah Wali, Nahodilová, Radmila, Dolejš, David (2010) Incipient eclogite facies metamorphism in the Moldanubian granulites revealed by mineral inclusions in garnet. Lithos, 114 (1) 54-69 doi:10.1016/j.lithos.2009.07.014
Plain TextFaryad, Shah Wali, Nahodilová, Radmila, Dolejš, David (2010) Incipient eclogite facies metamorphism in the Moldanubian granulites revealed by mineral inclusions in garnet. Lithos, 114 (1) 54-69 doi:10.1016/j.lithos.2009.07.014
In(2010, January) Lithos Vol. 114 (1) Elsevier BV

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Nahodilová, Radmila, Faryad, Shah Wali, Dolejš, David, Tropper, Peter, Konzett, Jürgen (2011) High-pressure partial melting and melt loss in felsic granulites in the Kutná Hora complex, Bohemian Massif (Czech Republic) Lithos, 125 (1) 641-658 doi:10.1016/j.lithos.2011.03.017
Faryad, Shah Wali, Jedlicka, Radim, Collett, Stephen (2013) Eclogite facies rocks of the Monotonous unit, clue to Variscan suture in the Moldanubian Zone (Bohemian Massif) Lithos, 179. 353-363 doi:10.1016/j.lithos.2013.07.015
Hrouda, František, Faryad, Shah Wali, Jeřábek, Petr, Chlupáčová, Marta, Vitouš, Petr (2009) Primary magnetic fabric in an ultramafic body (Moldanubian Zone, European Variscides) survives exhumation-related granulite-amphibolite facies metamorphism. Lithos, 111 (1) 95-111 doi:10.1016/j.lithos.2008.10.004
Jedlicka, Radim, Faryad, Shah Wali (2017) Felsic granulite with layers of eclogite facies rocks in the Bohemian Massif; did they share a common metamorphic history?. Lithos, 286. 408-425 doi:10.1016/j.lithos.2017.06.027
Kulhánek, Jan, Faryad, Shah Wali (2023) Compositional changes in garnet: trace element transfer during eclogite-facies metamorphism. Contributions to Mineralogy and Petrology, 178 (10) doi:10.1007/s00410-023-02050-8
Faryad, Shah Wali, Kachlík, Václav, Sláma, Jiří, Jedlicka, Radim (2016) Coincidence of gabbro and granulite formation and their implication for Variscan HT metamorphism in the Moldanubian Zone (Bohemian Massif), example from the Kutná Hora Complex. Lithos, 264. 56-69 doi:10.1016/j.lithos.2016.08.005
Perraki, Maria, Faryad, Shah Wali (2014) First finding of microdiamond, coesite and other UHP phases in felsic granulites in the Moldanubian Zone: Implications for deep subduction and a revised geodynamic model for Variscan Orogeny in the Bohemian Massif. Lithos, 202. 157-166 doi:10.1016/j.lithos.2014.05.025
Kulhánek, Jan, Faryad, Shah Wali, Jedlicka, Radim, Svojtka, Martin (2021) Dissolution and Reprecipitation of Garnet during Eclogite-facies Metamorphism; Major and Trace Element Transfer during Atoll Garnet Formation. Journal of Petrology, 62 (11) doi:10.1093/petrology/egab077
Faryad, Shah Wali, Ježek, Josef (2019) Compositional zoning in garnet and its modification by diffusion during pressure and temperature changes in metamorphic rocks; an approach and software. Lithos, 332. 287-295 doi:10.1016/j.lithos.2019.03.002
Faryad, Shah Wali (2009) The Kutná Hora Complex (Moldanubian zone, Bohemian Massif): A composite of crustal and mantle rocks subducted to HP/UHP conditions. Lithos, 109 (3) 193-208 doi:10.1016/j.lithos.2008.03.005
Žák, Jiří, Verner, Kryštof, Finger, Fritz, Faryad, Shah Wali, Chlupáčová, Marta, Veselovský, František (2011) The generation of voluminous S-type granites in the Moldanubian unit, Bohemian Massif, by rapid isothermal exhumation of the metapelitic middle crust. Lithos, 121 (1) 25-40 doi:10.1016/j.lithos.2010.10.002
 
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