Vanadinite and desclozite of secondary lead minerals occur in a cave between the ovelying dolomite marble and the se ricitecale schist at the bottom of the Keban metamorphic massive, Elazığ county East Turkey.
📌 3 Key Takeaways
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Objective & Hypothesis:Vanadinite and desclozite of secondary lead minerals occur in a cave between the ovelying dolomite marble and the se ricitecale schist at the bottom of the Keban metamorphic massive, Elazığ county East Turkey.
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Key Findings & Data:Vanadinite and desclozite of secondary lead minerals occur in a cave between the ovelying dolomite marble and the se ricitecale schist at the bottom of the Keban metamorphic massive, Elazığ county East Turkey.
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Conclusion & Impact:Vanadinite and desclozite of secondary lead minerals occur in a cave between the ovelying dolomite marble and the se ricitecale schist at the bottom of the Keban metamorphic massive, Elazığ county East Turkey.
🔬Design:Araştırma Makalesi
📍Scope:Comprehensive Sample
⚙️Variables:Vanadinit · Desklozit
Abstract
Vanadinite and desclozite of secondary lead minerals occur in a cave between the ovelying dolomite marble and the se ricitecale schist at the bottom of the Keban metamorphic massive, Elazığ county East Turkey.
Özet
Sekonder kurşun minerallerinden olan vanadinit ve desklozit birbirinden farklı mineralojik özelliklere sahiptir. Her iki mineralde görülen zonlanma, oluşum esnasında kimyasal bileşimde değişimler meydana geldiğini ortaya koyar. Minerallerin kimyasal formülüne giren vanadyumun fillitlerden; kurşun, çinko ve bakırın ise ana sülfid yatağından geldiği anlaşılmıştır. Sekonder yatak yanal salgı neticesinde meydana gelmiş litojen bir oluşumdur.