Origin and nature of the mineralizing fluids of thrust zone fluorites in Celikhan (Adiyaman, Eastern Turkey): A geochemical approach

Sasmaz A., Onal A., Sagiroglu A., Onal M., Akgul B.

GEOCHEMICAL JOURNAL, cilt.39, sa.2, ss.131-139, 2005 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 39 Sayı: 2
  • Basım Tarihi: 2005
  • Doi Numarası: 10.2343/geochemj.39.131
  • Dergi Adı: GEOCHEMICAL JOURNAL
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.131-139
  • İnönü Üniversitesi Adresli: Hayır

Özet

The Celikhan fluorite mineralization is concentrated in the thrust zone between the Ptnarbast Formation, which forms the hanging wall, and the Kalecik Limestone foot wall. Fluorite occurs as fracture fills in the thrust zone and as replacement of the foot wall. The wall rock alteration consists of calcite, barite, quartz and kaolinite.