Mircovski, Vojo and Boev, Blazo and Spasovski, Orce (1996) The amphibolite rocks south-west of the village of Mitrashinci, the Serbo-Macedonian massif, Republic of Macedonia. Terranes of Serbia. pp. 173-178.
Preview |
Text
geologic_frameworkBoev3.pdf Download (2MB) | Preview |
Abstract
An elongated zone of amphibolite rocks with iron-titanium mineralization was discovered in the Precambrian metamorphic complex southwest of the village of Mitrashinci. Based all their mineralogical and chemical composition two types of amphibolites were distiguished: garnet-cummingtonite or irontitanium as well as garnet-biotite or aluminium sodium type. The amphibole of the cummingtonite types was determined for the first time by our investigations. The mineral assemblages and the chemical composition of the horblende, garnet and biotite
indicate that the main metamorphic phase took place under conditions of almandine amphibolite facies at T of550 +/- 50 "c and P from 4 to 6 kbar.
Item Type: | Article |
---|---|
Uncontrolled Keywords: | amphibolite, garnet, hornblende, cummingtonite, biotite, metamorphism |
Subjects: | Natural sciences > Other natural sciences |
Divisions: | Faculty of Natural and Technical Sciences |
Depositing User: | Vojo Mircovski |
Date Deposited: | 03 Dec 2012 15:06 |
Last Modified: | 10 Jun 2013 09:32 |
URI: | https://eprints.ugd.edu.mk/id/eprint/2957 |
Actions (login required)
View Item |