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OCCURRENCE OF LEAD-ZINK ORE AT Mt. IVANŠČICA NEAR IVANEC (CROATIA)

Boris Šinkovec
Ladislav Palinkaš
Goran Durn


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Abstract

Mineral and ore occurences at Mt. Ivanščica are situated in the Middle Triassic carbonate rocks and are of epigenetic origin. These occurences are characterised by simple paragenesis of primary sulphides of leads and zinc and traces of sulphides of iron and copper. This mineralization is similar to Mississippi Valley Pb-Zn deposits.

Keywords

lead-zinc ore; Mt. Ivanščica; epigenetic mineralization; Mississippi Valley Pb-Zn deposits

Hrčak ID:

5028

URI

https://hrcak.srce.hr/5028

Publication date:

4.12.2000.

Article data in other languages: croatian

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