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Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt
Archives for Technical Sciences, (2021), 24; 17-30. https://doi.org/10.7251/afts.2021.1324.017s
Salkić, Zehra; Babajić, Elvir; Lugović, Boško

Institucijski repozitorij: Repozitorij Rudarsko-geološko-naftnog fakulteta Sveučilišta u Zagrebu

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Salkić, Z., Babajić, E. i Lugović, B. (2021). Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt. Archives for Technical Sciences, (24), 17-30. doi: 10.7251/afts.2021.1324.017s

Salkić, Zehra, et al. "Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt." Archives for Technical Sciences, br. 24, 2021, str. 17-30. https://doi.org/10.7251/afts.2021.1324.017s

Salkić, Zehra, Elvir Babajić i Boško Lugović. "Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt." Archives for Technical Sciences br. 24 (2021): 17-30. https://doi.org/10.7251/afts.2021.1324.017s

Salkić, Z., Babajić, E. i Lugović, B. (2021) 'Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt', Archives for Technical Sciences, (24), str. 17-30. doi: 10.7251/afts.2021.1324.017s

Salkić Z, Babajić E, Lugović B. Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt. Archives for Technical Sciences [Internet]. 2021. [pristupljeno 29.11.2024.];(24):17-30. doi: 10.7251/afts.2021.1324.017s

Z. Salkić, E. Babajić i B. Lugović, "Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt", Archives for Technical Sciences, br. 24, str. 17-30, 2021. [Online]. Dostupno na: https://urn.nsk.hr/urn:nbn:hr:169:353141. [Citirano: 29.11.2024.]

Za citiranje koristite ovu mrežnu adresu: https://urn.nsk.hr/urn:nbn:hr:169:353141
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Naslov (engleski)Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt
Naslov (engleski)Geochemistry and petrogenesis of Oligocene dacites from the Central Bosnia and Herzegovina with insight in the post-collisional tectonic evolution of Central Dinaridic Ophiolite Belt
AutorZehra Salkić
AutorElvir Babajić
AutorBoško Lugović
MBZ: 58780
Autorova ustanovaSveučilište u Zagrebu
Rudarsko-geološko-naftni fakultet
(Zavod za mineralogiju, petrologiju i mineralne sirovine)
Znanstveno / umjetničko
područje, polje i grana		PRIRODNE ZNANOSTI
Geologija
Sažetak (engleski)
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 (southernmost distal outcrops) or geological setting (extrusive within the melange of the Internal Dinaride Ophiolite Belt). Major element composition of the CBTVR reveals high-K calc-alkaline geochemical affinity whereas trace element discriminate the rocks as shoshonitic. The rocks are LILE-enriched and show negative Ta-Nb, P and Ti anomalies, and positive Pb anomalies typical of subduction related volcanic rocks. Chondrite-normalized REE patterns exhibit significant LREE/HREE enrichment [(La/Yb)(cn) = 21.4 - 33.4]. Geochemical affinity of the CBTVR combined with tectonic position of extrusions suggests derivation of the melts from the subcontinental mantle which had inherited strong orogenic signature during an ancient subduction.
Ključne riječi (engleski)
Jezikengleski
Vrsta publikacijeZnanstveni rad - Izvorni znanstveni rad
Status objaveObjavljen
Vrsta recenzijeRecenziran - međunarodna recenzija
Verzija publikacijeObjavljena verzija rada (izdavačev PDF)
Naslov časopisaArchives for Technical Sciences
Brojčani podacibr. 24, str. 17-30
p-ISSN2233-0046
DOIhttps://doi.org/10.7251/afts.2021.1324.017s
URN:NBNurn:nbn:hr:169:353141
Datum objave publikacije2021
URL dokumentahttps://doisrpska.nub.rs/index.php/arhivzatehnickenauke/article/view/7252
Vrsta resursaTekst
Prava pristupaOtvoreni pristup
Uvjeti korištenjaIkona licence Zaštićeno autorskim pravom.
Datum i vrijeme pohrane2023-02-17 12:11:19