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Original scientific article

IMPORTANCE OF OLISTOSTROME MEMBER FOR METALLOGENY OF LJUBIJA IRON ORE DEPOSITS

By
Aleksandar Grubić ,
Aleksandar Grubić
Contact Aleksandar Grubić

Academy of Sciences and Arts of Republika Srpska Bosnia and Herzegovina

Ranko Cvijić ,
Ranko Cvijić

Mining Institute Prijedor , Prijedor , Bosnia and Herzegovina

Aleksej Milošević ,
Aleksej Milošević

Mining Faculty, University of Banja Luka , Banja Luka , Bosnia and Herzegovina

Miodrag Čelebić
Miodrag Čelebić

Mining Faculty, University of Banja Luka , Banja Luka , Bosnia and Herzegovina

Abstract

Ljubija mining area is built of more formations that belong to the Carboniferous, Permian, Triassic and Cenozoic. From all of these, only two are metalliferous to iron: Javorik formation with olistostrome member and Neogene-Quaternary of Prijedor basin. The first includes primary siderite and ankerite partially limonitised ore and in the second only redeposited limonite (limonite pieces and dust, known under the commercial name "brand"). Appearance of iron is also in other members of Javorik formation and other formations, but these are just thin veins. They have no significance for the economic exploitation but are an important element in the interpretation of metallogeny in the region. These findings came from many years of fieldwork and synthesis of all published and unpublished data related to iron ore in this area.

Therefore, this work gives special importance to olistostrome member, its stratigraphic position and metallogenic characteristics.

References

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Citation

This is an open access article distributed under the  Creative Commons Attribution Non-Commercial License (CC BY-NC) License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. 

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