Gümüşhane ÜniversitesiGümüşhane ÜniversitesiAçık Erişim Arşivi · RDL Open

Ore Mineralogical Study of Cerattepe Au-Cu (±Zn) VMS Deposit (Artvin-Turkey)

Kitap BölümüAçık Erişim

Özet

The Cerattepe mine, one of the volcanogenic massive sulfide deposits in northeastern Turkey, is hosted within the late Cretaceous volcanic, intrusive and sedimentary rocks. Deposit’s main ore body contains high-grade massive copper sulfides and a gold-silver and barium rich oxide zone, characterized by dense alteration stages, is situated on top of it. Replacement, cataclastic, breccia, dissemination, dendritic, concentric growth, colloform, and framboidal textures were identified. Pyrite, sphalerite, marcasite, chalcopyrite, bornite, galena, tennantite-tetrahedrite, gold, covellite, digenite, chalcocite, cuprite and cubanite constitute the mineral paragenesis where quartz, calcite and barite account for the gangue minerals. Limonite, hematite, lepidocrocite, malachite, azurite and jarosite developed in the oxidation zone.

Anahtar Kelimeler

Bird’s eye-textureCerattepeEastern PontideFramboidal pyriteVMS deposit
RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/gumushane/12988Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.1007/978-3-030-22974-0_2Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorAkpınar, I.
dc.contributor.authorÇiftçi, E.
dc.contributor.editorGlagolev, S
dc.date.accessioned2026-10-22T10:20:47.629487747Z
dc.date.available2026-10-22T10:20:47.629487747Z
dc.date.issued2019
dc.description.abstractThe Cerattepe mine, one of the volcanogenic massive sulfide deposits in northeastern Turkey, is hosted within the late Cretaceous volcanic, intrusive and sedimentary rocks. Deposit’s main ore body contains high-grade massive copper sulfides and a gold-silver and barium rich oxide zone, characterized by dense alteration stages, is situated on top of it. Replacement, cataclastic, breccia, dissemination, dendritic, concentric growth, colloform, and framboidal textures were identified. Pyrite, sphalerite, marcasite, chalcopyrite, bornite, galena, tennantite-tetrahedrite, gold, covellite, digenite, chalcocite, cuprite and cubanite constitute the mineral paragenesis where quartz, calcite and barite account for the gangue minerals. Limonite, hematite, lepidocrocite, malachite, azurite and jarosite developed in the oxidation zone.
dc.description.sponsorshipIstanbul Technical University in Turkey
dc.description.sponsorshipBritish Association for Psychopharmacology, BAP, (39615)
dc.identifier.doi10.1007/978-3-030-22974-0_2
dc.identifier.eissn2524-3438
dc.identifier.endpage10
dc.identifier.isbn978-3-030-22974-0
dc.identifier.isbn978-3-030-22973-3
dc.identifier.issn2524-342X
dc.identifier.scopus2-s2.0-85101260804
dc.identifier.startpage7
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/12988
dc.identifier.wosWOS:000554403800002
dc.language.isoen
dc.publisherSpringer Nature
dc.relation.conference14th International Congress for Applied Mineralogy (ICAM)
dc.relation.ispartofSpringer Proceedings in Earth and Environmental Sciences
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectBird’s eye-texture
dc.subjectCerattepe
dc.subjectEastern Pontide
dc.subjectFramboidal pyrite
dc.subjectVMS deposit
dc.subject.classificationMineralogy
dc.subject.classificationMining & Mineral Processing
dc.titleOre Mineralogical Study of Cerattepe Au-Cu (±Zn) VMS Deposit (Artvin-Turkey)
dc.typeBook Chapter
dspace.entity.typePublication
rdl.citation.openalex4
rdl.citation.scopus3
rdl.citation.wos4
rdl.conference.dateSEP 23-27, 2019
rdl.conference.placeBelgorod Technol Univ, Belgorod, RUSSIA
rdl.oa.statushybrid
rdl.oa.urlhttps://link.springer.com/content/pdf/10.1007%2F978-3-030-22974-0_2.pdf
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexConference Proceedings Citation Index - Science (CPCI-S)