Abstract
The Arapuçandere Pb-Zn-Cu ores are typical examples of vein-type lead-zinc deposits in the Biga Peninsula. Permian—Triassic metamorphic, Triassic metaclastic and metabasic rocks, Oligocene—Miocene granitoids, Miocene volcanic rocks, and Quaternary terrestrial sediments crop out in the study area. The veins occupy fault zones in Triassic metasandstone (meta-arkose and subarkose) and metadiabase, and contain galena, sphalerite, chalcopyrite, pyrite, marcasite, covellite and specular hematite as ore minerals, with quartz, calcite, and barite as gangue minerals. Based on macro- and micro-petrographic investigations, sulfide minerals formed in the earliest stage of mineralization, and were followed by quartz and calcite crystallization. Fluid inclusion studies showed that salinity (avg. 18.3%) was low, but that temperature was relatively high (avg. 301.4°C) during stages of sulfide precipitation. In contrast, the salinity (avg. 27.1% NaCl equiv.) increased and the temperature (avg. 240.2°C) decreased during crystallization of the quartz. Finally, the salinity and temperature of the fluid gradually declined through the later episode of mineralization when the primary and secondary inclusions in calcite formed. Isotopic compositions of the aqueous fluid (δ18O = -7.5 to -1.7%, and δD = -90 to -55%) indicate the presence of meteoric water modified slightly by fluid-rock interaction. A geologic and genetic relation between ore veins and Oligo-Miocene granitoids and Miocene volcanic rocks appears to be lacking. The ore and host-rock relations suggest only a post-Triassic age for the mineralization. Pb-isotope model ages suggest a pre-Eocene age for the mineralization, which predated Oligo-Miocene granitoid emplacement and Miocene volcanic activity. We conclude that the Pb-Zn-Cu veins in the study area formed by deeply circulating meteoric water. The metals and sulfur were leached from the surrounding pre-Eocene units and deposited along fault zones.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
