Mircovski, Vojo (2002) Amphibolitic rocks of the lower precambrian matamorphic complex of the Pelagonian massif. Geologica Carpathica, Proceedings of the XVII Congress of Carpatian-Balkan geological association, 53.
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Abstract
Amphibolitic rocks have been found near Stavica in the central part of the Pelagonian massif. They are made up of hornblende, garnet, diopside, epidode, zoisite, albite-oligoclase, biotite as well as titanite muscovite and quartz as accessory minerals. Amphipolites were metamorphosed in polymetamorphic processes that took part in three metamorphic phases.
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | Diopside, garnet, epidode, amphibolites, Stavica |
| Subjects: | Natural sciences > Other natural sciences |
| Divisions: | Faculty of Natural and Technical Sciences |
| Depositing User: | Vojo Mircovski |
| Date Deposited: | 21 Dec 2012 08:41 |
| Last Modified: | 11 Jun 2013 13:41 |
| URI: | https://eprints.ugd.edu.mk/id/eprint/4180 |
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