Doğanşehir (Malatya)’da ki Barit Cevherleşmelerinin Kökeni: İz ve Nadir Toprak Element, İzotop ve Sıvı Kapanım Bulguları

Abstract

Bu çalışmada, Doğu Toroslar'da yer alan Doğanşehir (Malatya) barit cevherleşmesinin jeokimyasal ve izotopik özellikleri ortaya konmuştur. Gözlenen bu barit cevherleşmeleri metamorfik kayaçların çatlak zonları içinde yer almaktadır. Çalışma alanındaki baritlerin eser element verileri, Ba, Pb ve Zn'nin farklı kaynaklardan türetilmiş olabileceğini göstermektedir: bu elementler muhtemelen çalışma alanındaki rekristalize kireçtaşlarından ve silisli kayalardan gelmektedir. REE ve CeN / SmN'ye karşı CeN / YbN diyagramındaki barit değerlerinin grafikleri, deniz suyunun bariti çökelten hidrotermal sıvıya hükmettiğini ve baryum ve sülfat iyonlarını sağlarken, akışkan bir deniz suyu karışımı sağladığını göstermektedir. Pb izotop çalışmaları (206Pb / 204Pb = 17.04-19.2; 207Pb / 204Pb = 14.33-17.00 ve 208Pb / 204Pb = 34.19-41.66), baritteki kurşunun manto, orojen ve kabuktan türetildiğini ve taban kayaları tarafından hafifçe kirlendiğini göstermektedir. Kükürt izotopik çalışmaları, baritteki kükürtün deniz suyu sülfat kaynaklarından türetildiğini göstermektedir (δ34SVCDT değerleri 17,5 ‰ ila 30,7 ‰ arasındadır). Barit örneklerinde yapılan mikrotermometrik çalışmalar, 85 ° C ile 122 ° C arasında değişmekte, ortalama 110 ° C olduğu belirlenmiştir. Tuzluluklar ağırlıkça % 0,2 ila 2,6 NaCl arasında değişmektedir. İncelenen sıvı kapanımlarının homojenleşme sıcaklıkları, muhtemelen epitermal koşullarda oluşmuş olduğunu düşündürmektedir.

Keywords

• barit
• Kurşun izotopu
• sülfür izotopu
• sıvı kapanım

Origin of Barite Mineralization in the Doğanşehir (Malatya): Trace and Rare Earth Element, Isotope and Fluid Inclusion Evidence

Abstract

This study the main objective presented the geochemical and isotopic characteristics of the barite mineralization at the Doğanşehir (Malatya), located in the Eastern Taurids. These barite mineralizations observed are included in crack zones of metamorphic rocks. Trace element data of barite in the study area show that Ba, Pb and Zn may have been derived from different sources: these elements probably come from recrystallized limestones and siliceous rocks in the study area. The trends of the REE and the plots of the values of barites on the CeN/SmN versus CeN/YbN diagram indicate that seawater dominated the hydrothermal fluid depositing the barite and supplied the barium and sulfate ions, while a fluid mixture of seawater. Pb isotope studies (206Pb/204Pb=17.04-19.2; 207Pb/204Pb=14.33-17.00 and 208Pb/204Pb=34.19-41.66) indicate that the lead in barite was derived from the mantle, orogen, and crust and was slightly contaminated by the basement rocks. Sulfur isotopic studies indicate that the sulfur in barite has been derived from seawater sulfate sources (δ34SVCDT values range from 17.5 ‰ to 30.7 ‰). Microthermometric studies on barite samples range from 85°C to 122°C, with an average of 110°C. Salinities vary from 0.2 to 2.6 NaCl wt%. Homogenization temperatures of the studied fluid inclusions suggest which were probably formed in epithermal conditions.

Keywords

• barite
• lead isotope
• sulphur isotope
• fluid inclusion

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