Occurrence of Native Platinum and PGE-bearing Pyrite in the Porphyry-Skarn-Epithermal Ore Complex at Recsk, Hungary

  • Máté Biró Department of Mineralogy, Eötvös Loránd University
  • Dr. Molnár Ferenc Department of Mineralogy, Eötvös Loránd University
  • Hugh O'Brien Geological Survey of Finland - GTK
Keywords: platinum, PGE, porphyry, mineralization, native platinum, trace element, pyrite

Abstract

In this short report we present the first detection of a platinum group element (PGE) mineral and Cu-bearing native platinum in a hydrothermal breccia pipe in the intermediate sulfidation mineralization of the Recsk ore complex in Hungary. Trace element analyses of pyrite provide further insights into the enrichment of PGE in the mineralized complex.
The occurrence of native platinum is associated with one of the highest observed Pt contents in pyrite, as well as with other ore minerals such as Sn- and Pt-bearing native copper, pure native copper, and Ag-bearing tenorite. Crocoite and vanadinite were identified by SEM-EDS as secondary minerals possibly from the same paragenesis. Our new results suggest that the Recsk complex might contain economic PGE resources.

Author Biographies

Máté Biró, Department of Mineralogy, Eötvös Loránd University

matebiro.bm@gmail.com

Dr. Molnár Ferenc, Department of Mineralogy, Eötvös Loránd University

molnar.ferenc@ttk.elte.hu | https://orcid.org/0000-0002-1873-1915

Hugh O'Brien, Geological Survey of Finland - GTK

hugh.obrien@gtk.fi | https://orcid.org/0000-0002-7900-579X

Published
2023-11-12
Section
Articles