Journals / Maden Tetkik ve Arama Dergisi / 2012 / Cilt: 144 - Sayı: 144

THE GEOLOGY, GEOCHEMISTRY AND GENETICAL FEATURES OF THE ORMANBAŞI HILL (SİNCİK, ADIYAMAN) COPPER MINERALIZATION

Pages
75–104
Publication Date
2012-01-01
DOI
—
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

These values are both compatible with sulfur ratios in hydrothermal solutions related to volcanism and show a similar composition with that of Cyprus type VMS deposits on the world.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The study area covers Ormanbaşı Hill of Adıyaman–Sincik County and its vicinity.
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Key Findings & Data:Besides, analyses carried out in massive pyrites indicated that these had Ni/Co ratio higher than 1% and less Ni content.
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Conclusion & Impact:These values are both compatible with sulfur ratios in hydrothermal solutions related to volcanism and show a similar composition with that of Cyprus type VMS deposits on the world.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Adıyaman · Sincik · Koçali complex

Abstract

The study area covers Ormanbaşı Hill of Adıyaman–Sincik County and its vicinity. Regional geological locations of Cu mineralizations that lie between the Southeastern Anatolian Foothill Belt and Taurus Orogenic Belt are conformable with thrust planes approximately extending in E-W directions. Cu mineralizations are observed in the form of lenses and layers within mudstone, diabase, spilite, and claystone - shales of the Koçali complex. The primary genetic relations of these formations have completely been disappeared but have only been traced along thrust planes that are conformable with general tectonic lineaments. The ore structure is generally massive but is stockwork and disseminated in some zones. The ore-bearing layer with pyrite towards deeper parts is observed, while the mineralization is observed in the form of iron ore cap (gossan) at the surface. Ore paragenesis consists of pyrite, marcasite, chalcopyrite, sphalerite, bornite, chalcocite - covelline and native copper. All samples belonging to ore mineralizations plot on Cyprus type volcanogenic massive sulfide (VMS) area in Cu – Pb - Zn and Au - (Cu + Pb + Zn) - Ag ternary diagrams. All samples in Pb, Cu, Ag, Au and Zn spider diagrams which were normalized to primary mantle show a trend similar to VMS deposits. Besides, analyses carried out in massive pyrites indicated that these had Ni/Co ratio higher than 1% and less Ni content. Therefore; it was detected that hydrothermal processes had been effective in ore mineralizations. S32 /S34 ratios were obtained as 6.9 and 7.6 in sulfur isotope analyses performed by using pyrite and chalcopyrite samples. These values are both compatible with sulfur ratios in hydrothermal solutions related to volcanism and show a similar composition with that of Cyprus type VMS deposits on the world.

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Cite This Article

YILDIRIM, N., İLHAN, S., YILDIRIM, E., DÖNMEZ, C. (2012). THE GEOLOGY, GEOCHEMISTRY AND GENETICAL FEATURES OF THE ORMANBAŞI HILL (SİNCİK, ADIYAMAN) COPPER MINERALIZATION. Maden Tetkik ve Arama Dergisi, Cilt: 144 - Sayı: 144, 75–104. https://ajindex.com/articles/54082

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References (8)

  1. Altınlı, İ. E., 1966. Doğu ve Güneydoğu Anadolu’nun jeolojisi. MTA Bulletin, 66, 35-74.
  2. Barrie, C. T. and Hannington, M. D., 1999. Classification of volcanic-associated massive sulfide deposits based on host-rock composition. Reviews in Economic Geology, v. 8, 1-11.
  3. Bekar, K., 2010. Adıyaman – Sincik – Ormanbaşı Tepe Sahasının IP Yöntemi ile Araştırılması. 3. Yer Elektrik Çalıştayı, Genişletilmiş Özet Kitabı, Ankara Üniversitesi Ilgaz ÖRSEM Tesisleri, Çankırı, 24-26 Mayıs 2010.
  4. Beyarslan, M., Bingöl, A. F. and Yıldırım, N., 2009. Koçali Ofiyolitik Karmaşığının petrolojik ve tektono-magmatik özellikleri (Adıyaman). Tübitak Project (107Y344). (unpublished). Bingöl, A.F., 1993 a. Çermik-Çüngüş ve Dicle Yöresi Magmatik Kayaçlarının Petrografik Özellikleri. F.Ü. Fen Bilimleri Enstitüsü Fen ve Müh. Bilimleri Dergisi, 5/1, 1-9. ————, 1993 b. Çermik Yöresinde Koçali Karmaşığı’nın Jeokimyası. Doğa ve Yer Bilimleri Dergisi, 55-61.
  5. Boynton, W.V., 1984. Cosmochemistry of the rare earth elements: meteorite studies. In: Henderson, P. (Ed.), Rare Earth Element Geochemistry. Elsevier, Amsterdam, 63– 114. Campel, B. and Jorkovsky, J., 1967. Geochemie der Pyrite einiger Lagerstätten der Tschechoslowakei. VSAV Bratislava, 493p. Cengiz, R., 1991. Doğanşehir Malatya Yöresinin Jeolojisi Maden Jeolojisi ve Jeokimyası. Maden Tetkik ve Arama Genel Müdürlüğü, Report No: 10317, Ankara (unpublished). Clark, L.A., 1971. Volcanogenic ores: compar- ison of cupriferous pyrite deposits of Cyprus and Japanese Kuroko deposits. Soc. Mining Geologists Japan, Special Issue 3, 206-215.
  6. Constantinou, G. and Govett, G.J.S., 1973. Geology, geochemistry and genesis of Cyprus sulfide deposits. Economic Geology 68, 843-858.
  7. Galley A.G. and Koski, R.A., 1999. Setting and characteristics of ophiolite-hosted vol- canogenic massive sulphide deposits in Barrie, C.T., and Hannington, M.D., eds., Volcanic-Associated Massive Sul- phide Deposits: Processes and Examples in Modern and Ancient Settings: Reviews in Economic Geology, v. 8, 215-236.
  8. Güleç, N. and Erler, A., 1983. Masif sülfit yataklarındaki piritlerin karakteristik iz element içerikleri. TJK Bulletin, 26, 2, 145- 152. Gültekin, B., 2004. Sincik (Adıyaman) yöresi bakır ve altın içeren kuvars damarlarının oluşumu ve kökeni. Yüksek Lisans Tezi, Hacettepe Üniversitesi Fen Bilimleri Enstitüsü, Ankara (unpublished). Hannington, M.D., Galley, A.G., Herzig, P.M. and Petersen, S., 1998. Comparison of the TAG mound and stockwork complex with Cyprus-type mass