Composition of Pancarli Magmatic Ni-Cu +/-(PGE) Sulfide Deposit in the Cadomian-Avalonian Belt, Eastern Turkey

Yildirim E., Yildirim N., Donmez C., Gunay K., Korkmaz T., AKYILDIZ M., ...Daha Fazla

JOURNAL OF EARTH SCIENCE, cilt.31, sa.3, ss.536-550, 2020 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 31 Sayı: 3
  • Basım Tarihi: 2020
  • Doi Numarası: 10.1007/s12583-020-1299-5
  • Dergi Adı: JOURNAL OF EARTH SCIENCE
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Academic Search Premier, Aerospace Database, Agricultural & Environmental Science Database, Aquatic Science & Fisheries Abstracts (ASFA), CAB Abstracts, Communication Abstracts, Geobase, INSPEC, Metadex, Civil Engineering Abstracts
  • Sayfa Sayıları: ss.536-550
  • Anahtar Kelimeler: Ni-Cu +/-(PGE) sulfide deposit, delta S-34 isotopes, Neoproterozoic, Andean type, eastern Turkey, PLATINUM-GROUP ELEMENTS, MONOSULFIDE SOLID-SOLUTION, VOISEYS BAY, EXTERNAL SULFUR, FRACTIONAL CRYSTALLIZATION, CHINA IMPLICATIONS, ISOTOPIC EVIDENCE, STABLE-ISOTOPE, CURACA VALLEY, CU
  • Çukurova Üniversitesi Adresli: Evet

Özet

Pancarli Ni-Cu +/-(PGE) sulfide deposit occurs in the Neoproterozoic basement complex of the Bitlis massif, which is one of the Andean-type active continental margin fragments with arc-type assemblages represented by the Cadomian orogenic belt. Pancarli sulfides are associated with quartzo-feldspathic gneisses (country rock) and mafic intrusions (host rock). Composed of only semi-massive ore, the Ni-Cu +/-(PGE) sulfide deposit is a small-scale deposit, and it does not contain net-textured and disseminated ore. The mineral assemblage comprises pyrrhotite, pentlandite, and chalcopyrite. The semi-massive ore samples contain 2.2 wt.%-2.9 wt.% Ni, 0.8 wt.%-2.2 wt.% Cu (Cu/(Cu+Ni)=0.2-0.5) and 0.13 wt.%-0.17 wt.% Co. The Cu/Ni ratios (average 0.57) are consistent with the segregation of sulfides from a basaltic magma. Low Pt+Pd(100%S)values of 0.08 ppm-0.89 ppm, relatively low Pt/Pd ratios of 0.2-1.4, and Pd/Ir ratios of 4.5-39 have also been revealed. These values demonstrate that the magma reached S saturation before its emplacement and the mineralization with high Cu/Pd ratios formed by sulfides segregated from a PGE-depleted magma. delta S-34 isotope values (average -3.1 parts per thousand) of Pancarli sulfides are lower than mantle source. Negative delta S-34 value indicates contamination from surrounding rocks. Concerning the composition, remobilization style and magma type, the Pancarli Ni-Cu +/-(PGE) sulfide deposit is similar to the deposits associated with Andean-type magmatic arcs located in the convergent plate margin settings.