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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| Principais autores: | , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Faculty of Mining and Geology, Belgrade
2016-01-01
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| Serier: | Geološki Anali Balkanskoga Poluostrva |
| Fag: | |
| Online adgang: | http://www.doiserbia.nb.rs/img/doi/0350-0608/2016/0350-06081677013G.pdf |
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