| ZULAUF, Gernold, Wolfgang DORR, Jiří FIALA, Jana KOTKOVÁ, Henri MALUSKI a Pablo VALVERDE-VAQUERO. Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic). Terra Nova. Oxford: Blackwell Science Ltd., 2002, roč. 14, č. 5, s. 343-353. ISSN 0954-4879. |
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@article{483128,
author = {Zulauf, Gernold and Dorr, Wolfgang and Fiala, Jiří and Kotková, Jana and Maluski, Henri and ValverdeandVaquero, Pablo and Maluski, Henri and ValverdeandVaquero, Pablo},
article_location = {Oxford},
article_number = {5},
keywords = {Erzgebirge crystalline complex; North Bohemian shear zone; orthogneisses; granulites; structures; microfabric; diffusional creep; high temperature; U-Pb monazite dating; Ar-Ar mica dating; rapid cooling and exhumation},
language = {eng},
issn = {0954-4879},
journal = {Terra Nova},
title = {Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic).},
volume = {14},
year = {2002}
}
TY - JOUR
ID - 483128
AU - Zulauf, Gernold - Dorr, Wolfgang - Fiala, Jiří - Kotková, Jana - Maluski, Henri - Valverde-Vaquero, Pablo - Maluski, Henri - Valverde-Vaquero, Pablo
PY - 2002
TI - Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic).
JF - Terra Nova
VL - 14
IS - 5
SP - 343
EP - 343
PB - Blackwell Science Ltd.
SN - 09544879
KW - Erzgebirge crystalline complex
KW - North Bohemian shear zone
KW - orthogneisses
KW - granulites
KW - structures
KW - microfabric
KW - diffusional creep
KW - high temperature
KW - U-Pb monazite dating
KW - Ar-Ar mica dating
KW - rapid cooling and exhumation
N2 - Diffusional creep structures in orthogneisses and granulites of the North Bohemia shear zone (eastern part of the Erzgebirge crystalline complex)imply high interfacial free energy that has been preserved from equilibration as a result of rapid cooling. U-Pb dating of monazite and Ar-Ar dating of muscovite of Kadan orthogneisses result in a high cooling rate. This is consistent with a rapid tectonic movements, resulting in the juxtaposition of upper crustal rocks of the Tepla-Barrandian unit against lower crustal rocks of the Erzgebirge crystalline complex.
ER -
ZULAUF, Gernold, Wolfgang DORR, Jiří FIALA, Jana KOTKOVÁ, Henri MALUSKI a Pablo VALVERDE-VAQUERO. Evidence for high-temperature diffusional creep preserved by rapid cooling of lower crust (North Bohemian shear zone, Czech Republic). \textit{Terra Nova}. Oxford: Blackwell Science Ltd., 2002, roč.~14, č.~5, s.~343-353. ISSN~0954-4879.
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