Publication details

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

Authors

ZULAUF Gernold MALUSKI Henri DORR Wolfgang VALVERDE-VAQUERO Pablo FIALA Jiří KOTKOVÁ Jana MALUSKI Henri VALVERDE-VAQUERO Pablo

Year of publication 2002
Type Article in Periodical
Magazine / Source Terra Nova
MU Faculty or unit

Faculty of Science

Citation
Field Geology and mineralogy
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
Description 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.

You are running an old browser version. We recommend updating your browser to its latest version.

More info