Journals / Maden Tetkik ve Arama Dergisi / 2026 / Cilt: 164 Sayı: 164

Geology of the Yeşilyurt gold deposit: an example of low-angle normal fault related mineralization, Eastern Anatolia-Turkey

Esra Yıldırım(Fırat University, Department of Geological Engineering, Elazığ 23000, Turkey.)0000-0002-0823-988X
Nail Yıldırım(IV. Regional Directorate of Mineral Research and Exploration, Malatya 44100,Turkey)0000-0001-7459-5746
Cahit Dönmez(General Directorate of Mineral Research and Exploration, Ankara 06800, Turkey)0000-0003-4705-9301
Kurtuluş Günay(Marmara Regional Directorate of Mineral Research and Exploration, Kocaeli, Turkey)0000-0002-3358-1185
Pages
261–279
Publication Date
2021-04-15
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AI Summary & Key Takeaways

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

This deposit will lead to finding new gold deposits in Eastern Taurus Orogenic Belt.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:Yeşilyurt gold mineralization is located within the provincial borders of Malatya and Adıyaman in the East Anatolian Region.
📊
Key Findings & Data:Alteration assemblages are: (1) silica replacements/veinlets and, (2) quartz-pyrite replacements / veinlets.
💡
Conclusion & Impact:This deposit will lead to finding new gold deposits in Eastern Taurus Orogenic Belt.
🔬Design:Araştırma Makalesi
📍Scope:Comprehensive Sample
⚙️Variables:Yeşilyurt gold mineralization · Detachment fault/Lowangle normal fault · Fault gauge

Abstract

Yeşilyurt gold mineralization is located within the provincial borders of Malatya and Adıyaman in the East Anatolian Region. This mineralization is one of the gold deposits which correlated with low-angle normal/detachment fault. Low-angle normal fault associated with a tectonic setting which is potential extensional in Paleogene-Neogene (?) term. Marble-recrystallized limestone which belongs to the metamorphic core is the dominant rock (footwall) type in the bottom plate of the fault zone. There are deformed graphitic calc-schists (hanging wall) in the upper plate of the fault zone. The fault zone is characterized by fault gauge, cataclasite, and breccia. While the cataclasite, and breccia are the principal ore host, there is weaker mineralization in fault gauge. Alteration assemblages are: (1) silica replacements/veinlets and, (2) quartz-pyrite replacements / veinlets. High gold contents are closely related to silicification and quartz-pyrite alteration which damaged the primary textures. Small volume syn-tectonic magmatic rocks are simultaneous and typically monitored in the silicified areas which are border on the high-grade gold mineralization. Mineralization is a non-base metalliferous Au depositthat contains Au/Ag ~ 1.07, As (~0.27%), F (1.59%), and a trace amount of Sb. This deposit will lead to finding new gold deposits in Eastern Taurus Orogenic Belt.

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Cite This Article

Yıldırım, E., Yıldırım, N., Dönmez, C., Günay, K. (2021). Geology of the Yeşilyurt gold deposit: an example of low-angle normal fault related mineralization, Eastern Anatolia-Turkey. Maden Tetkik ve Arama Dergisi, Cilt: 164 Sayı: 164, 261–279. https://doi.org/10.19111/bulletinofmre.797729

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