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mélange of Zlatibor Mt.(SW Serbia) – age and geodynamic implicationsNATAŠA GERZINA1 & NEVENKA DJERIĆ2Abstract. Cherts are quite frequently occurring rocks in the Internal Dinarides, an extremely complex areacomposed of several

ophiolites and partly metamorphosed parts of the distal continental margin of Adria are preserved. Therefore, these cherts differ in age andthe original depositional environment in which they were formed.Results of investigations

the mélange in the vicinity of Jasenovovillage on SE slopes of Zlatibor Mt. are presented here. Radiolarian cherts from the studied localities represent blocks in mélange of the East-Bosnian–Durmitor Unit, exposed in a large