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Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye)

Yıl 2022, Cilt: 169 Sayı: 169, 63 - 85, 05.12.2022
https://doi.org/10.19111/bulletinofmre.1074485

Öz

Magmatic processes that emerged with the evolution of the Neotethys ocean and associated lithospheric plates caused the formation of significant mineralization in the Tethys belt. The Eastern Pontides, which are located in the northeast of Türkiye and are a part of the Tethys metallogenic belt, are particularly rich in porphyry-type mineralization and represent an important region for Cu-Mo exploration. A large number of Cu, Pb and Zn anomalies have been determined in a large region including the Güzelyayla Cu-Mo field by stream sediment sampling. The Güzelyayla occurrence is Cu-Mo mineralization associated with andesitic/basaltic volcanic rocks and intrusive dacites crosscutting these rocks. The Güzelyayla Cu-Mo mineralization developed in the stockwork and fault-controlled silicified zones. Homogenization temperature values vary between 324 °C and 420 °C (average 374 °C). Salinity values range between 2.2 and 18.6% NaCl (average 9.1% NaCl). A concentric alteration zoning surrounding the potassic alteration indicates a gradual change in the physicochemical properties of the solutions forming the mineralization. The Güzelyayla mineralization was formed in the Eocene (50.7 ± 1.0 million years) period in the Upper Cretaceous volcanic rocks in relation to post-collisional processes in the magmatic arc environment. Contrary to previous studies, estimation zone models were created and an estimated 54.2 million tons of extracted/potential mineral resource with an average grade of 0.20% Cu and 0.014% Mo (0.26% Cu equivalent grade) was made in the Güzelyayla field.

Destekleyen Kurum

This article includes the studies carried out within the scope of the project (project no: 2017/2018/2019- 32-13-12) titled Gümüşhane ve Çevresi Metalik Maden Aramaları (Gümüşhane and Surrounding Metallic Mineral Explorations) by MTA. We would like to thank the geological engineers Abdullah DURSUN and Arif Çağrı SUBAŞI who accompanied us in the field studies carried out within the scope of the project.

Proje Numarası

project no: 2017/2018/2019- 32-13-12

Teşekkür

We would like to thank the geological engineers Abdullah DURSUN and Arif Çağrı SUBAŞI who accompanied us in the field studies carried out within the scope of the project.

Kaynakça

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Yıl 2022, Cilt: 169 Sayı: 169, 63 - 85, 05.12.2022
https://doi.org/10.19111/bulletinofmre.1074485

Öz

Proje Numarası

project no: 2017/2018/2019- 32-13-12

Kaynakça

  • Akaryalı, E., Tüysüz, N. 2013. The genesis of the slab window-related Arzular low-sulfidation epithermal gold mineralization (eastern Pontides, NE Turkey). Geoscience Frontiers 4, 409421.
  • Arslan, M., Kolaylı, H., Temizel, I. 2004. Petrographical, geochemical and petrological characteristics of the Güre (Giresun, NE Turkey) Granitoid. Bulletin of Earth Sciences Application and Research Centre of Hacettepe University 30, 121.
  • Aslan, N. 2011. Mastra (Gümüşhane) Yatağı’nın jeolojik, mineralojik ve jeokimyasal özellikleri. Yüksek Lisans Tezi. Karadeniz Teknik Üniversitesi, Fen Bilimleri Enstitüsü, Trabzon, 190s. (yayımlanmamış).
  • Aydın, F. 2014. Geochronology, geochemistry, and petrogenesis of the Maçka subvolcanic intrusions: implications for the Late Cretaceous magmatic and geodynamic evolution of the eastern part of the Sakarya zone, northeastern Turkey. International Geology Review 56, 1246–1275.
  • Aydın, F., Saka, S.O., Şen, C., Dokuz, A., Aiglsperger, T., Uysal, İ., Kandemir, R., Karslı, O., Sarı, B., Başer, R. 2020. Temporal, geochemical and geodynamic evolution of the Late Cretaceous subduction zone, NE Turkey: Implications for mantle-crust interaction in an arc setting. Journal of Asian Earth Sciences 192, doi.org/10.1016/j.jseaes.2019.104217.
  • Aydınçakır, E., Şen, C. 2013. Petrogenesis of the post-collisional volcanic rocks from the Borçka (Artvin) area: implications for the evolution of the Eocene magmatism in the Eastern Pontides (NE Turkey). Lithos 172-173, 98117.
  • Bektaş, O., Yılmaz, C., Taslı, K., Akdağ, K., Özgür, S. 1995. Cretaceous rifting of the eastern Pontides carbonate platform (NE Turkey): the formation of the carbonate breccias and turbidites as evidence of a drowned platform. Giarnale di Geologica 57, 233244.
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  • Revan, M.K., Maslennikov, V.V., Genç, Y., Delibaş O., Maslennikova, S.P. Sadykov, S.A. 2016. Sulfur isotope study of the vent chimneys from the Upper Cretaceous VMS deposits of the eastern Pontide metallogenic belt, NE Turkey. Turkish Journal of Earth Sciences 25, 227241.
  • Revan, M.K., Hisatani K., Miyamoto H., Delibas O., Hanilçi N., Aysal N., Özkan M., Çolak T., Karslı Ş., Peytcheva I. 2017. Geology, U-Pb geochronology, and stable isotope geochemistry of the Tunca semi-massive sulfide mineralization, NE Turkey: Implications for ore genesis. Ore Geology Reviews 89, 369389.
  • Revan, M.K., Genç, Y., Delibaş, O., Maslennikov, V.V., Nuriya, R.A., Zimitoğlu, O. 2019. Mineralogy and geochemistry of metalliferous sedimentary rocks from the upper Cretaceous VMS deposits of the eastern Pontides (NE Turkey). Turkish Journal of Earth Sciences 28, 299327.
  • Revan, M.K. 2021. A review of Late Cretaceous volcanogenic massive sulfide mineralization in the Eastern Pontides, NE Turkey. Turkish Journal of Earth Sciences 29, 11251153.
  • Rice, S.P., Robertson, A.H.F., Ustaömer, T., İnan, N., Taslı, K. 2009. Late Cretaceous-early Eocene tectonic development of the Tethyan suture zone in the Erzincan area, Eastern Pontides, Turkey. Geological Magazine 146, 567590.
  • Richards, J.P. 2014. A review of tectonics and metallogeny of the Tethyan orogen. Acta Geologica Sinica 88, 923925.
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  • Schultze-Westrum, H.H. 1961. Giresun civarındaki Aksu deresinin jeolojik profili; Kuzeydoğu Anadolu’da, Doğu Pontus cevher ve mineral bölgesinin jeolojisi ve maden yatakları ile ilgili mütalaalar. Maden Tetkik ve Arama Dergisi 57, 6371.
  • Seedorff, E., Dilles, J.H., Proffett, J.M., Jr., Einaudi, M.T., Zurcher, L., Stavast, W.J.A., Johnson, D.A., Barton, M.D., 2005. Porphyry deposits: characteristics and origin of hypogene features: In: Hedenquist, J.W., Thompson, J.F.G., Golfarb, R,J., Richards, J.R., (Eds). Society of Economic Geologists, Economic Geology 100th Anniversary Volume, 1905–2005, p. 251–298.
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  • Soylu, M. 1999. Modeling of porphyry copper mineralization of the Eastern Pontides. PhD thesis. Middle East Technical University, Ankara 127p.
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Toplam 88 adet kaynakça vardır.

Ayrıntılar

Birincil Dil İngilizce
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Mustafa Kemal Revan Bu kişi benim 0000-0001-9395-8389

Deniz Göç Bu kişi benim 0000-0002-6204-5314

Mustafa Özkan Bu kişi benim 0000-0002-0872-8739

Cüneyt Şen Bu kişi benim 0000-0002-2873-073X

Rasim Taylan Kara Bu kişi benim 0000-0002-3675-9049

Mustafa Tokoğlu Bu kişi benim 0000-0001-8760-4488

Semi Hamzaçebi Bu kişi benim 0000-0001-8719-9160

Rıfat Cihan Sevim Bu kişi benim 0000-0003-1218-9544

Fatih Sezen Bu kişi benim 0000-0003-4515-564X

Celaleddin Bayraktar Bu kişi benim 0000-0002-3941-9445

Ömer Akgül Bu kişi benim 0000-0003-2794-3618

Proje Numarası project no: 2017/2018/2019- 32-13-12
Yayımlanma Tarihi 5 Aralık 2022
Yayımlandığı Sayı Yıl 2022 Cilt: 169 Sayı: 169

Kaynak Göster

APA Revan, M. K., Göç, D., Özkan, M., Şen, C., vd. (2022). Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye). Bulletin of the Mineral Research and Exploration, 169(169), 63-85. https://doi.org/10.19111/bulletinofmre.1074485
AMA Revan MK, Göç D, Özkan M, Şen C, Kara RT, Tokoğlu M, Hamzaçebi S, Sevim RC, Sezen F, Bayraktar C, Akgül Ö. Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye). Bull.Min.Res.Exp. Aralık 2022;169(169):63-85. doi:10.19111/bulletinofmre.1074485
Chicago Revan, Mustafa Kemal, Deniz Göç, Mustafa Özkan, Cüneyt Şen, Rasim Taylan Kara, Mustafa Tokoğlu, Semi Hamzaçebi, Rıfat Cihan Sevim, Fatih Sezen, Celaleddin Bayraktar, ve Ömer Akgül. “Geology, Fluid Inclusion Characteristics and Mineral Resource Estimation of the Güzelyayla Porphyry Cu-Mo Mineralization (NE Türkiye)”. Bulletin of the Mineral Research and Exploration 169, sy. 169 (Aralık 2022): 63-85. https://doi.org/10.19111/bulletinofmre.1074485.
EndNote Revan MK, Göç D, Özkan M, Şen C, Kara RT, Tokoğlu M, Hamzaçebi S, Sevim RC, Sezen F, Bayraktar C, Akgül Ö (01 Aralık 2022) Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye). Bulletin of the Mineral Research and Exploration 169 169 63–85.
IEEE M. K. Revan, “Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye)”, Bull.Min.Res.Exp., c. 169, sy. 169, ss. 63–85, 2022, doi: 10.19111/bulletinofmre.1074485.
ISNAD Revan, Mustafa Kemal vd. “Geology, Fluid Inclusion Characteristics and Mineral Resource Estimation of the Güzelyayla Porphyry Cu-Mo Mineralization (NE Türkiye)”. Bulletin of the Mineral Research and Exploration 169/169 (Aralık 2022), 63-85. https://doi.org/10.19111/bulletinofmre.1074485.
JAMA Revan MK, Göç D, Özkan M, Şen C, Kara RT, Tokoğlu M, Hamzaçebi S, Sevim RC, Sezen F, Bayraktar C, Akgül Ö. Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye). Bull.Min.Res.Exp. 2022;169:63–85.
MLA Revan, Mustafa Kemal vd. “Geology, Fluid Inclusion Characteristics and Mineral Resource Estimation of the Güzelyayla Porphyry Cu-Mo Mineralization (NE Türkiye)”. Bulletin of the Mineral Research and Exploration, c. 169, sy. 169, 2022, ss. 63-85, doi:10.19111/bulletinofmre.1074485.
Vancouver Revan MK, Göç D, Özkan M, Şen C, Kara RT, Tokoğlu M, Hamzaçebi S, Sevim RC, Sezen F, Bayraktar C, Akgül Ö. Geology, fluid inclusion characteristics and mineral resource estimation of the Güzelyayla porphyry Cu-Mo mineralization (NE Türkiye). Bull.Min.Res.Exp. 2022;169(169):63-85.

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