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Gürkuyu Sb Cevherleşmesinde (Gediz Kütahya Türkiye) Mineraoloji, Jeokimya ve Kararlı İzotop İncelenmesi

Mineralogy, Geochemistry and Stable Isotope Investigation of Gürkuyu Sb Mineralization (Gediz-Kütahya-NW Turkey)

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Abstract (2. Language): 
The Gürkuyu Sb mineralization is located in the western part of Anatolian tectonic belt, in southern part of İzmir- Ankara zone and in northern part of Menderes Massif. The mineralization located at west of the Koca hill in east of Gürkuyu village of Gediz (Kütahya-Turkey) has been characterized through the detailed examinations involving sulfur and oxygen isotope. Serpentinites of Dağardı melange and crystallized limestones of Budağan limestone were hydrothermally altered by hydrothermal solutions, come from fissures and fractures due to tectonic movement during the thrust of melange and occurred silicified zone. Gürkuyu Sb mineralization suggest that occurred in this silicified zone. In Gürkuyu mineralization, primary ore minerals are antimonite and pyrite, secondary ore minerals are senarmontite, valentinite, orpiment and realgar. Quartz and calcite are the most common gangue minerals. In mineralization, average contents of Fe2O3, Sb, Hg, As and Au are 2.15 wt.%, 13359 pm, 1.12 ppm, 1367 ppm and 163.82 ppb, respectively. In Gürkuyu Sb mineralization, δ34S values of stibnite are ranged from 1.0 ‰ to 1.3 ‰. δ18O values of quartz are ranged is 15.8 ‰ in Gürkuyu mineralization. Sulfur and oxygen isotope values are similar to the values for magmatic rocks and to the values for fluids of magmatic origin.
Abstract (Original Language): 
Gürkuyu Sb cevherleşmesi Anadolu tektonik kuşağının batısında, İzmir-Ankara zonunun güneyinde, Menderes Masifinin kuzeyinde yer almaktadır. Koca Tepe batısında, Gürkuyu Köyü (Gediz (Kütahya) güneyinde yer alan cevherleşmede mineraloji, jeokimya ve duraylı izotop (S,O) çalışmaları yapılmıştır. Dağardı melanjının bindirmesi esnasında ve daha sonra devam eden tektonik hareketlere bağlı olarak oluşan kırık ve çatlaklardan gelen hidrotermal çözeltilerin, Dağardı melanjına ait serpantinitlerle Budağan kireçtaşlarına ait kristalize kireçtaşlarını hidrotermal alterasyona uğratarak oluşan silisleşmiş zon içinde Gürkuyu antimonit cevherleşmesini meydana getirdiği düşünülmektedir. Gürkuyu cevherleşmesinde birincil cevher mineralleri antimonit ve pirit iken ikincil cevher mineralleri senarmontit, valentinit, orpiment ve realgardır. Kuvars ve kalsit ise en yaygın gang mineralleridir. Cevherleşmede Fe2O3, Sb, Hg, As ve Au değerleri sırasıyla % 2.15, 13359 pm, 1.12 ppm, 1367 ppm ve 163.82 ppb’dir. Gürkuyu Sb cevherleşmesinde antimonitin δ34S değerleri ‰ 1.0 ile ‰ 1.3 arasında değişmektedir. Kuvarsın δ18O değeri ise ‰ 15.8’dir. Sülfür ve oksijen izotop sonuçları magmatik kökenli sıvılar ve magmatik kayaçlardaki değerler ile benzerlik göstermektedir.
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