Alpine Plutono-Magmatism and Metamorphism in the South-Eastern Parts of the Vardar Zone and the Serbo­ - Macedonian Massif

Stojanov, Risto and Boev, Blazo (1997) Alpine Plutono-Magmatism and Metamorphism in the South-Eastern Parts of the Vardar Zone and the Serbo­ - Macedonian Massif. Proceeding Magmatism, Metaporphism and Metallogeny of the Vardar zone and Serbo - Macedonian massif.

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Abstract

Intense magmatic actlVlty and high temperature metamorphism took place in the subduction zone of the ophiolite complex in the south-eastern parts of the Vardar zone beneath the continental crust of the Serbo-Macedonian massif in the territory of the Republic of Macedonia and northern Greece to Chalkidiki during the Alpine period. The zone is characterized by charriage relationships of north-east dipping of formations present as Paleozoic, Mesozoic and Upper Eocene rocks. The presence of a diabase cherts formation of regional strike determined between Skopska Crna Gora and Chakidiki in the eastern parts of the Vardar zone is important. The presence of regional high temperature metamorphism, particularly manifested south-southeast of the town of Stip was determined. Uplift of blocks and discovery of the Stip granites (plutonic bodies) developed by melting of rocks of the earth's crust less than 10 krn in depth with halos of medium to high temperature migmatites and in low pressure conditions. To the south the zone extends over Mount Gradeski - Plaus and via Valandovo and Bogdanci continues further to the territory of Greece to the Peonias zone. The zone is tens of kilometers wide.

Item Type: Article
Subjects: Engineering and Technology > Other engineering and technologies
Natural sciences > Other natural sciences
Divisions: Faculty of Natural and Technical Sciences
Depositing User: Blazo Boev
Date Deposited: 03 Dec 2012 14:43
Last Modified: 19 Jun 2013 08:18
URI: http://eprints.ugd.edu.mk/id/eprint/2950

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