Publication details

Turmalíny ze svorů svrateckého krystalinika

Title in English Tourmaline from the mica schist of the Svratka Crystalline Complex
Authors

BURIÁNEK David ČOPJAKOVÁ Renata

Year of publication 2008
Type Article in Periodical
Magazine / Source Acta Mus. Moraviae, Sci. geol.
MU Faculty or unit

Faculty of Science

Citation
Field Geology and mineralogy
Keywords tourmaline; schorl-dravite; boron; metamorphism; mica schist; Svratka Crystalline Complex; Czech Republic
Description Tourmaline is a typical accessory mineral for most of micaschists in the Svratka Crystalline Complex. Based on petrographic and chemical data, two main generations of tourmaline have been distinguished. The first generation (tourmaline cores) corresponds to the prograde metamorphic event characterised by mineral assemblage Ms+Bt+Tu+/-Ky+/-St. The second generation of tourmaline (tourmaline rims) formed during exhumation of the Svratka Crystalline Complex, simultaneously with decompression breakdown of staurolite. Microprobe analyses of tourmalines reveal a compositional variation between Al-rich schorldravite to dravite (XFe 0.22-0.61; Al 5.88-6.77 apfu; Na 0.45-0.91 apfu). Tourmaline rims are typically enriched in Fe, usually enriched in Al and depleted in Mg, Na, Si relative to tourmaline cores.

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

More info