Metallogenic model of the Lykling ophiolite-hosted lode Au deposit, Scandinavian Caledonides: Insight from fluid inclusions, mineral chemistry and stable isotope geochemistry

[Display omitted] •The Lykling deposit represents an ophiolite-hosted orogenic Au mineralization type.•The mineralization occurs in forms of two generation of auriferous quartz veins.•The Lykling deposit documents three distinct stages of its formation.•Stable isotope geochemistry reveals a magmatic...

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Veröffentlicht in:Ore geology reviews 2024-10, Vol.173, p.106227, Article 106227
Hauptverfasser: Strmić Palinkaš, Sabina, Riple Forsberg, Frida, Birger Pedersen, Rolf, Hallås Stubseid, Håvard, McClenaghan, Seán H., Spangenberg, Jorge E.
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Sprache:eng
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