Published January 1, 2014 | Version v1
Journal article Open

Platinum group element (PGE) mineralisation and chromite geochemistry in the Berit ophiolite (Elbistan/Kahramanmaras), SE Turkey

  • 1. Gen Directorate Mineral Res & Explorat MTA, TR-06520 Ankara, Turkey
  • 2. Cardiff Univ, Cardiff CF10 3AT, S Glam, Wales
  • 3. Univ Min & Met Leoben, Chair Geol & Econ Geol, A-8700 Leoben, Austria
  • 4. Univ Karlsruhe, Inst Mineral & Geochem, D-76128 Karlsruhe, Germany

Description

The high-Al chromitite-bearing stratigraphic levels (Cr# ranges from 0.38 to 0.47) are located at the mantle/crust transition zone (MTZ) and in the cumulate dunites in the Berit ophiolite in SE Turkey. Iridium group elements-IPGE (Ir, Os and Ru) and related mineralisation were previously reported from ophiolitic high-Cr chromitites in the Berit-Elbistan area. Palladium group elements - PPGE (Pt, Pd and Rh) and associated mineralisation are predominantly found in the high-Al chromitites and they are presented in this study for the first time. Our results indicate that IPGE-enriched phases of the PGMs such as laurite are present in both the PPGE-enriched and the PPGE-poor chromitites in Berit.

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