Počet záznamů: 1
Strain coupling between upper mantle and lower crust: natural example from the Běstvina granulite body, Bohemian Massif
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SYSNO ASEP 0330511 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Strain coupling between upper mantle and lower crust: natural example from the Běstvina granulite body, Bohemian Massif Tvůrce(i) Machek, Matěj (GFU-E) ORCID, RID
Ulrich, Stanislav (GFU-E)
Janoušek, V. (CZ)Zdroj.dok. Journal of Metamorphic Geology. - : Wiley - ISSN 0263-4929
Roč. 27, č. 9 (2009), s. 721-737Poč.str. 17 s. Jazyk dok. eng - angličtina Země vyd. GB - Velká Británie Klíč. slova Bohemian Massif ; eclogite ; granulite ; peridotite ; strain coupling ; Variscan orogeny ; LPO Vědní obor RIV DB - Geologie a mineralogie CEP GA205/09/0539 GA ČR - Grantová agentura ČR CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000271523900009 DOI 10.1111/j.1525-1314.2009.00830.x Anotace Strain patterns within mantle rocks and surrounding coarse-grained felsic granulites from the Kutná Hora Crystalline Complex in the Variscan Bohemian Massif have been studied in order to assess their strain coupling. The studied rock association occurs within low-strain domains surrounded by finegrained granulite and migmatite. The Doubrava peridotite contains closely spaced and steeply dipping layers of garnet clinopyroxenite, which are parallel to the NE–SW-striking, high-temperature foliation in nearby granulites, while the Úhrov peridotite lacks such layering. The Spačice eclogite is not associated with peridotite and shows upright folds of alternating coarse- and fine-grained varieties bearing NE– SW-striking axial planes. Pracoviště Geofyzikální ústav Kontakt Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Rok sběru 2010
Počet záznamů: 1