Journals / Pamukkale Üniversitesi Mühendislik Bilimleri Dergisi / 2002 / Cilt: 8 - Sayı: 1

GEOLOGICAL AND GEOCHEMICAL FEATURES OF THE KIZILDAĞ (AKSEKİ- ANTALYA) CHROMITE OCCURRENCES

KIZILDAĞ (AKSEKİ-ANTALYA) KROMİTLERİNİN JEOLOJİK VE JEOKİMYASAL ÖZELLİKLERİ

Pages
97–102
Publication Date
2002-01-01
DOI
—
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AI Summary & Key Takeaways

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

There is a strong negative correlation between Cr and Mg and negative (not too strong) correlation between Cr and Al.

📌 3 Key Takeaways

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Objective & Hypothesis:The study area is located at 20 km southwest of Seydişehir (Konya) and the chromites are cropped out in the dunitic rocks of the Kızıldağ ultramafics.
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Key Findings & Data:These chromites can be classified as Al- rich and ferric chromites and their Cr/Fet is between 2.77 and 3.28 (mean 2.99).
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Conclusion & Impact:There is a strong negative correlation between Cr and Mg and negative (not too strong) correlation between Cr and Al.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Kromit · Ultramafik kayaç · Alpin tip

Abstract

The study area is located at 20 km southwest of Seydişehir (Konya) and the chromites are cropped out in the dunitic rocks of the Kızıldağ ultramafics. The chromites are found as banded, schliren and massive occurrences and their chemical composition have a features of Alpine type chromites. These chromites can be classified as Al- rich and ferric chromites and their Cr/Fet is between 2.77 and 3.28 (mean 2.99). In the Cr/Cr+AlMg/Mg+Fe +2 binary diagram, r/Cr+Al values covers a festricted area while Mg/Mg + Fe+2 ratios distrubuted in a wider range. There is a strong negative correlation between Cr and Mg and negative (not too strong) correlation between Cr and Al.

Özet

Seydişehir'in yaklaşık 20 km güneybatısında bulunan Kızıldağ'da ortaya çıkan kromitler ultramafik kütlenin dunit bileşimli kayaçları içerisinde bulunmaktadır. Bu kayaçlar içerisinde bandlı, saçılımlı ve masif yapılı olarak bulunan kromitler, kimyasal bakımdan Alpin tip kromitlerin özelliğini taşımaktadır. Al'lu ve Ferri kromit olarak adlandırılan kromitlerin Cr/Fet oranı 2.77 ile 3.28 arasında (ort. 2.92) değişmektedir. Cr/Cr+Al-Mg/Mg+Fe+2diyagramında üç değerlikli bileşenler dar bir alanda iki değerlikli bileşenler ise daha geniş bir alanda dağılım gösterirler.

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Cite This Article

DÖYEN, A., ZEDEF, V. (2002). GEOLOGICAL AND GEOCHEMICAL FEATURES OF THE KIZILDAĞ (AKSEKİ- ANTALYA) CHROMITE OCCURRENCES. Pamukkale Üniversitesi Mühendislik Bilimleri Dergisi, Cilt: 8 - Sayı: 1, 97–102. https://ajindex.com/articles/43297

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