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

I. Akpınar; E. Çiftçi

doi:10.1007/978-3-030-22974-0_2

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

I. Akpınar^*
, E. Çiftçi

^*Bu çalışma için yazışmadan sorumlu yazar

Jeoloji Mühendisliği Bölümü

Gumushane University

Araştırma sonucu: Kitap/Rapor/Konferans Bildirisinde Bölüm › Bölüm › bilirkişi

3 Atıf (Scopus)

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.

Orijinal dil	İngilizce
Ana bilgisayar yayını başlığı	Springer Proceedings in Earth and Environmental Sciences
Yayınlayan	Springer Nature
Sayfalar	7-10
Sayfa sayısı	4
DOI'lar	https://doi.org/10.1007/978-3-030-22974-0_2
Yayın durumu	Yayınlandı - 2019

Yayın serisi

Adı	Springer Proceedings in Earth and Environmental Sciences
ISSN (Basılı)	2524-342X
ISSN (Elektronik)	2524-3438

Bibliyografik not

Publisher Copyright:
© 2019, The Author(s).

Finansman

Acknowledgements. This study was financially supported by BAP Project unit (No: 39615) of Istanbul Technical University in Turkey. We are thankful to Mr. Ünsal Arkadaş and staff of Etibakır A.Ş. in Artvin, Turkey for their courteous support for the field work.

Finansörler	Finansör numarası
Istanbul Technical University in Turkey
British Association for Psychopharmacology	39615

Belgeye Erişim

10.1007/978-3-030-22974-0_2

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

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abstract = "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{\textquoteright}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.",

keywords = "Bird{\textquoteright}s eye-texture, Cerattepe, Eastern Pontide, Framboidal pyrite, VMS deposit",

author = "I. Akpınar and E. {\c C}ift{\c c}i",

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year = "2019",

doi = "10.1007/978-3-030-22974-0\_2",

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AU - Çiftçi, E.

PY - 2019

Y1 - 2019

N2 - 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.

AB - 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.

KW - Bird’s eye-texture

KW - Cerattepe

KW - Eastern Pontide

KW - Framboidal pyrite

KW - VMS deposit

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DO - 10.1007/978-3-030-22974-0_2

M3 - Chapter

AN - SCOPUS:85101260804

T3 - Springer Proceedings in Earth and Environmental Sciences

SP - 7

EP - 10

BT - Springer Proceedings in Earth and Environmental Sciences

PB - Springer Nature

ER -

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

Özet

Yayın serisi

Bibliyografik not

Finansman

Belgeye Erişim

Diğer Dosyalar ve Linkler

Parmak izi

Alıntı Yap