University of Isfahan Petrological Journal 2228-5210 3 11 2012 11 21 Investigation of the origin of Heneshk Hematitic iron deposit, Fars province using petrological, mineralogical and geochemical data Investigation of the origin of Heneshk Hematitic iron deposit, Fars province using petrological, mineralogical and geochemical data 19 38 16105 FA Mohhamad Ali Rajabzadeh Shervin Parvin Zohreh Moosavi Nasab Reza Shamsipour Dehkordi Journal Article 2016 06 14 Heneshk iron deposit is located between Gushti and Heneshk villages at Safashahr, NW of Fars province. Iron mineralization occurred as massive and lenticular shapes with silica and barite veins within brownish, silicified Triassic dolomitic host. Hematite and goethite are the principal ore minerals with minor magnetite that were formed through replacement and rarely open space filling within the host. Low concentrations of P ( Heneshk iron deposit is located between Gushti and Heneshk villages at Safashahr, NW of Fars province. Iron mineralization occurred as massive and lenticular shapes with silica and barite veins within brownish, silicified Triassic dolomitic host. Hematite and goethite are the principal ore minerals with minor magnetite that were formed through replacement and rarely open space filling within the host. Low concentrations of P ( https://ijp.ui.ac.ir/article_16105_928aea15b81cb42bf9e62798ec1d6bf2.pdf