Szczegóły publikacji

Opis bibliograficzny

Ore mineralogy, trace element distribution and 3D X-ray tomography of the polymetallic sulphide deposits at Mavres Petres and Piavitsa, Greece / Karin Högdahl, Erik Jonsson, Samuel Roško, Adam WŁODEK, Thomas Zack, Eric Landström, Edward P. Lynch, Fredrik Sahlström, Pavlos Tsitsanis, Vaggelis Bacalis // W: Life with Ore Deposits on Earth [Dokument elektroniczny] : 15th Biennial SGA Meeting, Glasgow, Scotland, August 27-30 2019 : proceedings. Vol. 1, Advances in understanding hydrothermal processes / University of Glasgow Publicity Services. — Wersja do Windows. — Dane tekstowe. — [Glasgow] : Society for Geology Applied to Mineral Deposits, cop. 2019. — e-ISBN: 978-0-85261-962-9. — S. 279–282. — Wymagania systemowe: Adobe Reader. — Tryb dostępu: https://www.dropbox.com/s/dqpnskg3xt0enbl/eVolume%201.pdf?dl=0 [2019-09-09]. — Bibliogr. s. 282, Abstr.

Autorzy (10)

  • Högdahl Karin
  • Jonsson Erik
  • Roško Samuel
  • AGHWłodek Adam
  • Zack Thomas
  • Landström Eric
  • Lynch Edward P.
  • Sahlström Fredrik
  • Tsitsanis Pavlos
  • Bacalis Vaggelis

Dane bibliometryczne

ID BaDAP123899
Data dodania do BaDAP2019-09-20
Rok publikacji2019
Typ publikacjimateriały konferencyjne (aut.)
Otwarty dostęptak
Konferencja15th Biennial SGA Meeting Life with Ore Deposits on Earth

Abstract

The Mavres Petres mine, operated by Hellas Gold, and the Piavitsa prospect are both located along the Stratoni fault in the Kassandra mining district, northern Greece. These Tertiary deposits are brecciated, carbonate replacement Pb-Zn-Ag-(Au) mineralisations and the Piavitsa deposit is also associated with Au-rich epithermal veins. Both mineralisations were variably overprinted by later fluids as well as ductile and brittle deformation affecting ore mineralogy and trace element distribution. Galena is the main Ag-carrier, contains significant concentrations of Sb and Bi and is locally associated with a suite of Sb-As-Bi phases. Sphalerite is either massive or occurs as a later cockade-textured type. Both varieties are variably enriched in Mn and can exhibit elevated concentrations of In and Ga. In Piavitsa, alabandite is present as small euhedral crystals or in veins in fractured sphalerite. Pyrite is ubiquitous and is either present as disseminations, massive to skeletal aggregates or as a matrix in breccias. It is often arsenic-bearing and even more so towards the later stages. Arsenopyrite appears to be a late phase and occurs interstitial to pyrite and as euhedral crystals. While both arsenopyrite and arsenian pyrite can be enriched in Au, As-minerals are not necessarily associated with Au.

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