Počet záznamů: 1
Ductile deformation and rheology of sub-continental mantle in a hot collisional orogeny: Example from the Bohemian Massif
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SYSNO ASEP 0365163 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Ductile deformation and rheology of sub-continental mantle in a hot collisional orogeny: Example from the Bohemian Massif Tvůrce(i) Kusbach, V. (CZ)
Ulrich, Stanislav (GFU-E)
Schulmann, K. (FR)Zdroj.dok. Journal of Geodynamics. - : Elsevier - ISSN 0264-3707
Roč. 56-57, May (2012), s. 108-123Poč.str. 16 s. Jazyk dok. eng - angličtina Země vyd. GB - Velká Británie Klíč. slova olivine lattice preferred orientation ; peridotite mylonite ; crust-mantle coupling ; Variscan orogen ; strain Vědní obor RIV DB - Geologie a mineralogie CEP GA205/09/0539 GA ČR - Grantová agentura ČR CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000302422700008 DOI 10.1016/j.jog.2011.06.004 Anotace Fabric patterns of strongly serpentinized peridotite were determined using eigenvector analysis and eigenvalue classification of lattice preferred orientation of olivine and orthopyroxene. This approach has been applied to a rootless fold-shaped body of mylonitized spinel to garnet peridotite surrounded by fine-grained and partially retrogressed ky–kfs granulite. The EBSD data show either axial [0 1 0] or [1 0 0](0 k l) pattern, both characteristic for ‘dry’ slip systems. The former pattern occurs predominantly along the inner margin and southern limb while the latter is mainly developed in the hinge of the fold shaped body. Pracoviště Geofyzikální ústav Kontakt Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Rok sběru 2013
Počet záznamů: 1