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The Haidbach deposit in the Central Tauern Window, Eastern Alps, Austria: a metamorphosed orthomagmatic Ni-Cu-Co-PGE mineralization in the Polymetallic Ore District Venediger Nappe System – Hollersbach Complex
Geology and Economic Geology, Montanuniversität Leoben, Peter-Tunnerstrasse 5, 8700 Leoben, Austria.
Urtelgasse 4, 2620 Neunkirchen, Austria.
Geology and Economic Geology, Montanuniversität Leoben, Peter-Tunnerstrasse 5, 8700 Leoben, Austria.
Analytical Chemistry, Montanuniversität Leoben, Franz-Josefstrasse 18, 8700 Leoben, Austria.
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2021 (English)In: Austrian Journal of Earth Sciences, ISSN 0251-7493, Vol. 114, no 1, p. 1-26Article in journal (Refereed) Published
Abstract [en]

Cu-Ni-Co-PGE mineralization occurs at Haidbachgraben in the Early Palaeozoic, Subpenninic Hollersbach Complex of the Central Tauern Window, Austria. Massive sulfide ore formed from sulfide melt segregated from silicate melt during intrusion of pyroxenite into magmatic rocks formed in an MORB-type environment. Relics of magmatic minerals include chromian spinel and polyphase sulfide droplets composed of pyrrhotite, chalcopyrite and pentlandite preserved in recrystallized pyrite. Both ore and host rocks were multiply deformed and metamorphosed, leading to hornblendite carrying the ore, enveloped by chlorite-epidote schist. Conditions of – likely Variscan – amphibolite facies metamorphism are documented by relict pargasitic cores in hornblende and actinolite-tremolite, and by ternary sulfarsenide compositions in the Co-Ni-Fe solid solution series that are the most common accessory minerals found in the sulfide ore. Pyrrhotite, pentlandite, chalcopyrite and pyrite are the major sulfide minerals. Chalcopyrite is Cd-rich and retains a high-temperature magmatic signature. High Co/Sb and moderate Se/As ratios in pyrite also point to a magmatic environment of mineralization. The accessory mineral assemblage of small grain size (mostly <10 µm) comprises native Au-Ag alloy and petzite as Au-Ag minerals, sperrylite, a variety of Pd tellurides and bismuthotellurides with elevated Sb, irarsite, and Re sulfides such as tarkianite and a Pb-Re sulfide. In addition, minor molybdenite, bournonite, scheelite and selenides have been identified. Two precious metal assemblages are present in individual samples: (1) hessite associated with Pd tellurides, often accompanied by sphalerite and chalcopyrite; (2) tarkianite forming euhedral inclusions in pyrite. Sperrylite and Au-Ag native alloys are present throughout and were also detected in silicate matrix. Most of the precious metal-bearing phases must have formed during recrystallization of base metal sulfides after the magmatic, and probably during later metamorphic events terminating in the Neoalpine Tauern crystallization.

Place, publisher, year, edition, pages
Walter de Gruyter, 2021. Vol. 114, no 1, p. 1-26
Keywords [en]
Nickel-copper sulfide ore, platinum-group minerals, rhenium sulfide, Hollersbach Complex, orthomagmatic sulfide deposit
National Category
Geochemistry
Research subject
Applied Geochemistry
Identifiers
URN: urn:nbn:se:ltu:diva-83495DOI: 10.17738/ajes.2021.0001ISI: 000624565400001Scopus ID: 2-s2.0-85105833577OAI: oai:DiVA.org:ltu-83495DiVA, id: diva2:1542187
Note

Validerad;2021;Nivå 2;2021-04-07 (alebob)

Available from: 2021-04-07 Created: 2021-04-07 Last updated: 2021-05-31Bibliographically approved

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Aiglsperger, Thomas

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