SEDIMENTARY LOW-MANGANESE HEMATITE DEPOSITS OF THE BUKOVICA AREA IN THE NORTHWESTERN MT. PETROVA GORA, CENTRAL CROATIA

Journal Title: UNKNOWN - Year 1998, Vol 10, Issue 1

Abstract

Middle-Permian Gröden deposits crop out on the surface of 0.8 km in the Bukovica area and on the surface of 0.8 km2 in the Mt. Loskun-jska gora in the NW part of the Petrova gora Mountain. One half of the Bukovica Gröden deposits contains in its lowest parts 1 to 5 m (in average 2.5 m) thick hematite bed cutted in blocks by NE-SW stretch¬ing vertical, normal and reverse faults. The hematite bed is unconfor-mably underlain by Lower Permian quartz-wackes (subgraywackes) intercalated with shales intercalations. Ore deposit is explored by 308 boreholes (10509 m) and by numerous adits, inclines and crosscuts on the underground surface of 0.4 km2 . From 1936 to 1941 and from 1953 to 1969 has been exploited 183000 t of ore with (in wt %): 34.0 Si02, 2.9 Al2O3; 59.0 Fe203; 0.15 MnO; 0.7 CaO; 0.4 MgO; 0.1 P, 0.37 S; 1.25 l.o. ign. Proven remaining ore reserves are 250.000 t. Paragenesis is investigated by microscopy of thin and polished sections, XRD, DTA, AAS analyses and by sedimentological analyses. Paragenesis major minerals are of hematite and quartz, with subordinate stable litho-clasts, muscovite (sericite) and scarce kaolinite, calcite, dolomite, and barite. Accessories are zircon, rutile, tourmaline, amphibole, garnet, apatite. Epigenetic veinlets and small nests are built up of quartz or calcite as the main neominerals associated with siderite, barite, kaolinite, pyrite, gypsum. Iron from the Bukovica hematite ore origi¬nated by land weathering during hot climate and transported by rivers and underground waters deposited in river beds, in flood plains and in shallow sea. Precipitation of the Bukovica iron ores took place after the Saalic orogenetic phase. At Hrastno (SE Slovenia) and at Rude nearby Samobor (Croatia), similar hematite deposits were found.

Authors and Affiliations

Milivoj Čop Ivan Jurković Dragutin Slovenec

Keywords

Related Articles

Živa u tlu i zraku kao element-indikator za boksitna ležišta u Istri - eksperimentalni istraživački model

U radu je obrađeno istraživanje sekundarne disperzije žive i nekih drugih elemenata oko boksitnih rudnih tijela u Istri. U tu svrhu izvršeno je uzorkovanje terra rosse uzduž traversi položenih preko boksitnih rudnih tije...

STUDIJA RASPODJELE U MODELU AKTIVACIJSKE ENERGIJE UPORABOM RAZLIČITIH FUNKCIJA RASPODJELE KOD PROBLEMA IZOTERMALNE PIROLIZE

Glavni cilj rada bio je usporedba rezultata dobivenih uporabom različitih vjerojatnosnih funkcija. Predviđen je model n-toga reda za model raspodjele aktivacijske energije (skr. MRAE), i to primjenom tehnike asimptotske...

CHARACTERIZATION OF METAL GRADES IN A STOCKPILE OF AN IRON MINE (CASE STUDY- CHOGHART IRON MINE, IRAN)

In any mining operation due to the cut-off grade (economic criteria), materials classify into the ore and waste. The material with grade equal to or higher than the cut-off grade is considered as ore and the material wit...

PROCJENA UČINKOVITOSTI POVRŠINSKE OBRADE PRIRODNOGA KAMENA UKRAJINE MEHANIČKIM I KEMIJSKIM METODAMA

Provedena su istraživanja s ciljem proučavanja načina poboljšanja ukrasnih svojstava proizvoda od prirodnoga kamena. To će omogućiti izradu završnoga proizvoda od prirodnoga kamena s homogenom bojom. U tu svrhu opisani s...

GEOTHERMAL ENERGY DEVELOPMENT STRATEGY IN REPUBLIC OF CROATIA DUE TO PROMOTION OF RENEWABLE ENERGY IN EUROPEAN UNION

According to European Strategy for sustainable, competitive and secure energy, which guidelines are described in two documents: ‘’Green Paper: a European Strategy for Sustainable, Competitive and Secure Energy’’ and ‘’Wh...

Download PDF file
  • EP ID EP29877
  • DOI -
  • Views 206
  • Downloads 3

How To Cite

Milivoj Čop Ivan Jurković Dragutin Slovenec (1998). SEDIMENTARY LOW-MANGANESE HEMATITE DEPOSITS OF THE BUKOVICA AREA IN THE NORTHWESTERN MT. PETROVA GORA, CENTRAL CROATIA. UNKNOWN, 10(1), -. https://europub.co.uk/articles/-A-29877