Mircovski, V. and Korikovsky, Sergey and Stojanov, Risto and Boev, Blazo (1997) Metamorphic Evolution and P -T Conditions of Eclogite -Amphibolites in the Buchim Block, Serbo -Macedonian Massif, Macedonia. Proceeding - Magmatism, Metamorphism and metallogency if the Vardar zone and Serbo-Macedonian massif.
Preview |
Text
proceeding_1997.pdf Download (2MB) | Preview |
Abstract
Microstructural characteristics and mineral assemblage indicate prograde and
retrograde stage in the metamorphic evolution of eclogite -amphibolites of the Buchim block. Based on Fe/Mg distribution between clinopyroxene and garnet and the content of Jd component in clinopyroxene, maximum T of
570 to 650°C and P of 12 - 12.5 Kbar were determined for prograde eclogitic stage. The increase of the content of anorthitic component in plagioclase of reaction symplectites as weII as progressive zoning in garnets surrounded by
hornblende - plagioclase symplectite indicates an increase of T in the initial stage of uplift, and later T get "normal" retrograde trend and decrease due to uplift movement. P - T condition determined that maximum depth at which metamor-phose took place ranges from 47 km (P == 12 - 12.5 Kbar)
that coincides to temperature gradient to 14°C/km.
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | eclogite -amphibolites, omphacite, garnet, plagioclase, thermo-metry, metamorphism |
| Subjects: | Engineering and Technology > Other engineering and technologies Social Sciences > Other social sciences |
| Divisions: | Faculty of Natural and Technical Sciences |
| Depositing User: | Blazo Boev |
| Date Deposited: | 03 Dec 2012 15:08 |
| Last Modified: | 21 Aug 2013 14:09 |
| URI: | https://eprints.ugd.edu.mk/id/eprint/2959 |
Actions (login required)
 |
View Item |