Go to main content | Go to main menu | Go to search

Project information
Tourmaline, dumortierite and their mineral assemblages as records of the melting process in B-rich peraluminous rocks from the Moldanubian zone

Information

This project doesn't include Faculty of Economics and Administration. It includes Faculty of Science. Official project website can be found on muni.cz.
Investor logo
Project Identification
GA205/99/0434
Project Period
1/1999 - 1/2001
Investor / Pogramme / Project type
Czech Science Foundation
  • Standard Projects
MU Faculty or unit
Faculty of Science
Cooperating Organization
The Moravian Museum Brno
  • Responsible person RNDr. Stanislav Houzar, Ph.D.

Tourmaline and less abundant dumortierite are typical minerals in magmatic and some high-grade metamorphic B-rich peraluminous rocks (leucocratic granites, migmatites, granitic pegmatites, granulites). They are commonly associated with AFM minerals (biot ite, cordierite, garnet) and Al2SiO5 polymorphs. Compositional variation in tourmaline, dumortierite and associated AFM minerals, phase relations and implication of relevant experimental studies of B-rich peraluminous systems published to date will provi de a basis for derivation of PTX-conditions and possible P-T paths in the studied tourmaline- and dumortierite-bearing rocks. Geochemical characteristics of parent rocks and PT data will characterize melting processes and related/subsequent metamorphism, thus contributing to our konwledge of geotectonic evolution of the Moldanubian Zone.

Publications

Total number of publications: 19

2004

2003

2002

Previous 1 2 Next

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