FORMATION MECHANISMS OF FE-MN CONCRETIONS IN THE VIJENAC QUARRY, DINARIC OPHIOLITE ZONE

FORMATION MECHANISMS OF FE-MN CONCRETIONS IN THE VIJENAC QUARRY, DINARIC OPHIOLITE ZONE

Vijenac quarry, near Tuzla in Bosnia-Herzegovina, is composed of carbonate rocks locally embedding tectonically disturbed siltite and sandstone with Mn-Fe concretions. The quarry itself represent a part of Dinaric overstep sequences (Pogari series) unconformably overlying ophiolite mélange and ophio...

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Bibliographic Details
Main Authors: Sibila Borojević Šoštarić, Srećko Bevandić, Tomislav Brenko, Elvir Babajić
Format: Article
Language:English
Published: Faculty of Mining, Geology and Petroleum Engineering 2018-01-01
Series:Rudarsko-geološko-naftni Zbornik
Subjects:
Fe-Mn concretions
diagenetic growth
Mn-minerals
chemical analysis
Dinaric Ophiolite Zone
Online Access:http://hrcak.srce.hr/file/295940

Internet

http://hrcak.srce.hr/file/295940

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