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Cherts are quite frequently occurring rocks in the Internal Dinarides, an   extremely complex area composed of several tectonostratigraphic units in   which oceanic sediments, ophiolites and partly metamorphosed parts of the   distal continental margin of Adria are preserved. Therefore, these cherts   differ in age and the original depositional environment in which they were   formed. Results of investigations carried out in the chert blocks found in   the melange in the vicinity of Jasenovo village on SE slopes of Zlatibor Mt.   are presented here. Radiolarian cherts from the studied localities represent   blocks in melange of the East-Bosnian-Durmitor Unit, exposed in a large   tectonic window below the Triassic carbonates of Drina-Ivanjica Unit.   Biostratigraphic data revealed Callovian-early Kimmeridgian ages of the   studied chert blocks, thus implying a Kimmeridgian or younger age of   obduction of the West Vardar ophiolites. [Projekat Ministarstva nauke   Republike Srbije, br. 176015

Chert blocks in the ophiolitic mélange of Zlatibor Mt. (SW Serbia): Age and geodynamic implications