Re-Os molybdenite ages of granitoid-hosted Mo-Cu occurrences from central Anatolia (Turkey)


DELİBAŞ O. , GENÇ Y.

ORE GEOLOGY REVIEWS, cilt.44, ss.39-48, 2012 (SCI İndekslerine Giren Dergi) identifier identifier

  • Yayın Türü: Makale / Derleme
  • Cilt numarası: 44
  • Basım Tarihi: 2012
  • Doi Numarası: 10.1016/j.oregeorev.2011.08.003
  • Dergi Adı: ORE GEOLOGY REVIEWS
  • Sayfa Sayıları: ss.39-48

Özet

The Central Anatolian Crystalline Complex (CACC), where many granitoids are emplaced and related ore occurrences/deposits occur, is tectonically located in the Alpine-Himalayan Belt The CACC hosts numerous ore occurrences/deposits (Cu, Mo, Fe, Pb and Zn) that are spatially associated with granitoids. The calc-alkaline Karacaali, Baliseyh and Basnayayla granitoids that form the northern granitoid belt of the CACC host important Mo-Cu occurrences. In this paper, we document Re-Os isotopic age data in molybdenites to determine the timing of the granitoid-hosted mineralizations in the CACC.