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 These findings came from many years of fieldwork and synthesis of all published and unpublished data related to iron ore in this area.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.
Janković S i J, R. Metallogeny of the Dinarides. Zbornik radova geologija i metalogenija Dinarida i Vardarske zone, str. 281-305. Akademija nauke i umjetnosti. 2000.
2.
Katzer F. Die Eisenerzvorrete Bosnie und der Hercegovina. Sonderband Berg und Huettenmann. Jahrbuch, Bd. 1910;58.
3.
Katzer F. Geologija Bosne i Hercegovine. Izdanje državnih rudarskih preduzeća u Sarajevu. 1926;
4.
Noeth L. Eisenerzlagerstaetten Jugoslawiens. Alger. 1952;2:529–63.
5.
Karamata S. Raspored ležišta gvozdenih ruda u svetlu geološke koncepcije tektonike ploča. Geološki glasnik br. 1976;21:17–29.
6.
Grubić A i P, Lj. Studija strukturnih i genetskih karakteristika tomašičkog rudnog polja. In: Cvijić, editori: Novi prilozi za geologiju i metalogeniju Rudnika gvožđa Ljubija Rudarski institut, Prijedor Prijedor. 2003. p. 63–137.
7.
Strmić-Palinkaš S, Spangeberg JE i P, A.L. Organic and inorganic geochemistry of Ljubija siderite deposits, NW Bosnia and Herzegovina. MinerDeposita, Springer-Verlag. 2009;44(8):893–913.
8.
Palinkaš AL. Siderite-barite-polysulfide deposits and early continental rifting in Dinarides. Geološki vjesnik, Zagreb. 1990;43:181–5.
9.
Palinkaš AL, Borojević S, Strmić S, Prochaska W, Spangeberg JE. Siderite-hematite-barite polysulfide mineral deposits, related to the Earlyintra –continental Tethyan rifting. In: Inner Dinarides U Eliopoulos i dr editori: Mineral Exploration and Sustainable Development, Millpress. 2003. p. 221–4.
10.
Strmić-Palinkaš S, Spangeberg JE, Palinkaš AL. Organic and inorganic geochemistry of Ljubija siderite deposits, NW Bosnia and Herzegovina. Miner Deposita, Springer-Verlag. 2009;44(8):893–913.
11.
Garašić V, Jurković I. Geochemical charasteristic of different iron ore types from the Southern Tomašica deposit, Ljubija, NW Bosnia. Geologia Croatica. 2012;65(2):255–70.
12.
Protić L i G, A. Paleozoic iron deposits in the Ljubija metallogenic district. Zbornik radova geologija i metalogenija Dinarida i Vardarske zone. Akademija nauke i umjetnosti Republike Srpske Banja Luka. :309–11.
13.
Katzer F. Geologija Bosne i Hercegovine. Izdanje državnih rudarskih preduzeća u Sarajevu. 1926;
14.
Jurić M. Geologija područja sanskog paleozoika u sjeverozapadnoj Bosni. Posebna izdanja Geološkog glasnika, knj. 1971.
15.
MarićL. CB. stijene sanskog paleozoika u rudnoj oblasti Ljubije. Geološki vjesnik. 1961;14.
16.
Jurković I. Minerali željeznih rudnih ležišta Ljubije kod Prijedora. Geološki vjesnik, br. 1961;14:161–220.
17.
Podubsky V. razvitak paleozoika u sjeverozapadnoj Bosni.Geološki glasnik, br. 12. 1969;165–95.
18.
Vasković N. Petrološka ispitivanja na uzorcima (iz Ljubije. Geoinstitut Beograd Ibid. 1984;1–30.
19.
Stefanovska D. Zaključci o rezultatima sedimentoloških ispitivanja karbonskog kompleksa. 1990;1–8.
20.
Šarac M. Metalogenetske karakteristike rudonosne oblasti Ljubije. Doktorska disertacija, Rudarsko-geološki fakultet u Beogradu. 1981;1–135.
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