Comparison of Epithermal Kaolin Deposits from the Etili Area (Çanakkale, Turkey): Mineralogical, Geochemical, and Isotopic Characteristics

被引:0
作者
Hatice Ünal Ercan
Ö. Işık Ece
Emin Çiftçi
Ayça Aydın
机构
[1] Konya Technical University,Chemistry and Chemical Processing Technologies
[2] Istanbul Technical University,Faculty of Mines
[3] University of Georgia,Department of Geology
来源
Clays and Clay Minerals | 2022年 / 70卷
关键词
Alunite; Hydrothermal alteration; Kaolinite; Silica sinter; Stable isotopes;
D O I
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中图分类号
学科分类号
摘要
Hydrothermal solutions related to magmatic intrusions that occurred during the Oligo-Miocene resulted in advanced multi-stage alterations and, to varying degrees, kaolinization over a wide area of the Biga Peninsula. The most important formations in these kaolin deposits occurred along the NE–SW-trending Çan-Etili-Bayramiç fault zone. The Bahadırlı, Duman, and Çaltıkara quarries are well preserved kaolin deposits throughout these fault zones located within the Çan Volcanics. Mineralogical, geochemical, and isotopic analyses were performed to identify the environments of formation of kaolins and the origin of the hydrothermal solution that led to the formation of these deposits.
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页码:753 / 779
页数:26
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