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The field, petrological-mineralogical, geochemical and geochronological data   of the metamorphic sole rocks recorded beneath the Fruška Gora, Povlen   (Tejići), Stolovi and Banjska ophiolites in the Western Vardar Zone (WVZ) and   beneath the Zlatibor, Bistrica, Sjenički Ozren and Brezovica ophiolites in   the Dinaridic ophiolite belt (DOB) in Serbia are compared. The focus has been   made on metabasic rocks formed in contact with the oceanic crust members:   cumulate gabbro and basalts of SSZ-type with E-MORB and OIB-signature and   more evolved tholeiitic basalts of MOR-affinity. Amphibole, the major phase   formed from the mafic sole components, depending on pressure-temperature   conditions exhibits compositional variations. According to mineral   assemblages, estimated P-T conditions and ages, the potential P-T paths are   given: high pressure - low temperature blueschist facies assemblage (7-9 kbar   and ~400°C and <300-350°C and 4-8 kbar), recorded only in the metamorphic   sole at the Fruška Gora (WVZ); high pressure - high temperature amphibolite   to granulite facies (8-10 kbar and >700-850°C), recorded in both domains, the   WVZ (Banjska) and the DOB (Bistrica, Sjenički Ozren, Brezovica) and medium   pressure - medium temperature amphibolite facies assemblages (~3.5-7 kbar and   >350-650°C) recognized in the WZV (Tejići, Devovići) and the DOB (Zlatibor).   The peak metamorphic conditions point to depths of the oceanic lithosphere   detachment and its initial cooling at 10-30 km, but the ages and tectonic   setting of ophiolites remain poorly constrained. The summarized data may be   used as an important key in geodynamic evolution of the Mesozoic Tethyan   ophiolites. [Projekat Ministarstva nauke Republike Srbije, br. 176019 and br.   176016

geološki anali balkanskoga poluostrva/geološki anali balkanskog poluostrva

Correlation of metabasic rocks from metamorphic soles of the Dinaridic and the Western Vardar zone ophiolites (Serbia): Three contrasting pressure-temperature-time paths