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Discrimination Criteria for Affiliation of Ore Deposits Located in the Dinaridic Triassic-Paleozoic Formations to the Variscan or Alpine Metallogeny

The important Dinaridic ore deposits are located in the Triassic (T)-Paleozoic (Pz) magmatic-metallogenic formations. Spatially, the ore deposits connected with Triassic rocks are genetically related to the Triassic gabbro-diorite-grano-syenite suite in intrusive level and basalt-andesite-dacite at extrusive level. Among many Pz terranes only Mid-Bosnian Mts. incorporate Upper Pz rhyolites, metamorphosed into metarhyolites. Within Pz formations the following types of ore deposits occur: type A polymetallic deposits formed in a broad pneumatolitic to epithermal interval ; type B stratabound carboniferous siderite± ankerite deposits with chalcopyrite ; type C Mid-Bosnian Mts. barite and barite-siderite deposits with Au- Hg-tetrahedrite ; type D monomineral barite occurrences with accessory sulphides.

Dinarides; Variscan metallogeny; Alpine metallogeny

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