Fluid evolution of mixed base-metal gold mineralization in the Tethys belt: Koru deposit, Turkey

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dc.contributor.authorBozkaya, Gulcan
dc.contributor.authorBozkaya, Omer
dc.contributor.authorBanks, David A.
dc.contributor.authorGokce, Ahmet
dc.contributor.editorMercierLangevin, P
dc.contributor.editorDube, B
dc.contributor.editorBardoux, M
dc.contributor.editorRoss, PS
dc.contributor.editorDion, C
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T09:44:04Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T09:44:04Z
dc.date.issued2017
dc.department[Bozkaya, Gulcan -- Bozkaya, Omer] Pamukkale Univ, Denizli, Turkey -- [Banks, David A.] Univ Leeds, Leeds, W Yorkshire, England -- [Gokce, Ahmet] Cumhuriyet Univ, Sivas, Turkeyen_US
dc.description14th SGA Biennial Meeting on Mineral Resources to Discover -- AUG 20-23, 2017 -- Quebec City, CANADAen_US
dc.description.abstractKoru is one of a number of base-metal gold deposits hosted by Oligo-Miocene volcano-sedimentary rocks of deposits in the Biga peninsula. Barite, quartz and galena are main minerals and are accompanied by minor amounts of sphalerite, pyrite, chalcopyrite, covellite and marcasite. Th of fluid inclusions indicates two distinct fluid pulses, one at high temperature (340 degrees C) commensurate with epithermal mineralization and boiling/near boiling conditions and the second approximately 150 degrees C lower. Salinity in both instances was from 11-0.2 wt. % NaCl. The range of temperatures within individual samples is consistent with variations from near lithostatic to hydrostatic pressure during vein and fracture opening. There are two different ranges of delta S-34 values of H2S in equilibrium with barite (+5.5 to +7.9 parts per thousand) and sulfide minerals (-2.1 to -0.5 parts per thousand), indicating that the sulfur in sulfide minerals and barite derived from different sources; magmatic and seawater respectively.en_US
dc.description.sponsorshipUniv Laval, Geol Survey Canada, Minist Energie & Ressources Naturelles Quebec, Inst Natl Rech Sci, Ctr Eau Terre Environm, DIVEX Network, Quebec Business Destinat, AREVA, OSISKO GOLD ROYALTIES, ABITIBI GEOPHYS, AngloAmerican, GOLDCORP, InnovExplo, INTEGRA GOLD CORP, ZEISS, COREM, Mira Geoscience, BARRICK, RESSOURCES 21, QUEBEC MINES, ios services GEOSCIENTIFIQUES inc, NEW BOLIDEN, KNOWLEDGE SCAPE, new gold, SGS, SOQUEM, Quebec Fonds Rech Nat Technol, srk consulting, stornowayen_US
dc.identifier.endpage286en_US
dc.identifier.isbn978-2-9816898-0-1
dc.identifier.startpage283en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12418/6894
dc.identifier.wosWOS:000439764100070en_US
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Scienceen_US
dc.language.isoenen_US
dc.publisherSOC GEOLOGY APPLIED MINERAL DEPOSITS-SGAen_US
dc.relation.ispartofMINERAL RESOURCES TO DISCOVER, VOLS 1-4en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titleFluid evolution of mixed base-metal gold mineralization in the Tethys belt: Koru deposit, Turkeyen_US
dc.typeConference Objecten_US

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