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

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 che...

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Bibliographic Details
Main Authors: Gerzina Nataša, Đerić Nevenka
Format: Article
Language:English
Published: Faculty of Mining and Geology, Belgrade 2016-01-01
Series:Geološki Anali Balkanskoga Poluostrva
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0350-0608/2016/0350-06081677013G.pdf