Geological, Geochemical and Microthermometric Characteristics of the Hakkari Region Zn-Pb Deposits, SE Turkey

Trace element associations (As, Se, Hg, Tl, Mn and Sb), fluid inclusion (Th from 165 to 289 °C; salinity from 1 to 22% equiv. NaCl) and isotope data indicate that the Hakkari Zn-Pb province were formed as synsedimentary processes associated with feeder systems during the initiation of the Triassic rifting in as a vent-proximal SEDEX-type.