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Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic)

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    0145540 - GLU-S 20023170 RIV GB eng J - Journal Article
    Zulauf, G. - Dörr, W. - Fiala, Jiří - Kotková, J. - Maluski, H. - Valverde-Vaquero, P.
    Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic).
    Terra Nova. Roč. 14, č. 5 (2002), s. 343-354. ISSN 0954-4879. E-ISSN 1365-3121
    R&D Projects: GA AV ČR KSK1012601
    Grant - others:DFG(DE) Zu73/1
    Keywords : North Bohemia * orthogneiss * rapid cooling
    Subject RIV: DB - Geology ; Mineralogy
    Impact factor: 0.874, year: 2002

    Volume diffusion and dislocation creep at T ~ 800 oCled to high finite strain in granulite and orthogneiss of the Ohře crystalline complex (North Bohemian shear zone). U-Pb dating of monazite (342+-4 Ma) of Kadaň orthogneiss result in a cooling rate of 50+25/-17 oC Myr -1.
    Permanent Link: http://hdl.handle.net/11104/0043117

     
     

Number of the records: 1  

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