CANADIAN MINERALOGIST, cilt.40, ss.895-908, 2002 (SCI-Expanded, Scopus)
Various types of celestine occurrences are hosted by Tertiary evaporite deposits and molasse-type sediments of the Sivas Basin, in east-central Anatolia, Turkey. Celestine mineralization occurs in various sedimentary facies, including elastic, carbonaceous and evaporitic. Mineralization in the Ba-Sr sulfate solid-solution series is found in a few samples from the Bahceciktepe celestine deposit, one of the typical mineralized sites in the Basin. Samples with a dendritic structure have karstic dissolution-induced voids and usually show a travertine-like texture; some are crystallized in fibroradial and subhedral tabular forms. In addition, clay envelopes around crystals and compositional and sector zoning of the crystals are typical features. XRD, electron-microprobe, single-crystal XRD and AAS analyses of the same samples suggest the presence of intermediate compositions in the BaSO4-SrSO4 solid-solution series, as well as compositions close to the end members.