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

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...

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Bibliographic Details
Main Authors: Boris Šinkovec, Ladislav Palinkaš, Goran Durn
Format: Article
Language:English
Published: Faculty of Mining, Geology and Petroleum Engineering 2000-12-01
Series:Rudarsko-geološko-naftni Zbornik
Subjects:
Online Access:http://hrcak.srce.hr/index.php?show=clanak&id_clanak_jezik=8098&lang=en
Description
Summary: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 (the paper is published in Croatian).
ISSN:0353-4529
1849-0409