Geochemistry and Petrogenesis of Oligocene Dacites From the Central Bosnia and Herzegovina With Insight in the Postcollisional Tectonic Evolution of Central Dinaridic Ophiolite Belt
Abstract:Magmatic rocks of post-Late Eocene magmatic formation are widespread in the Sava segment of Sava- Vardar suture zone and adjoin areas. The rocks formed as a response to transpressional-transtensional tectonic activity preceded by the Cretaceous-Eocene compression of the Internal Dinarides and Tisia Unit as fragments of Eurasian continental lithosphere. Central Bosnia Tertiary volcanic rocks (CBTVR), erupted as dacites in Lower Oligocene, are peculiar rocks of this formation either by their location (southernmo… Show more
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