Eski Arapgir (Malatya) civarındaki miyo-pliyosen birimlerin kil mineralojisi ve jeokimyası
Abstract
Çalışmada Alibona Formasyonu alt seviyeleri, üst seviyeleri ve Malatya Volkanitleri'yle girik durumda bulunan göl çökellerinden örnekleme yapılarak, çökellerin mineraloji ve jeokimyasının belirlenmesi amaçlanmaktadır. The Permo-Triassic Keban Metamorphics are characterized by marble with schists. Alibonca Formation overlies Keban Metamorphics with angular unconformities, and represented by shallow marine clayey-carbonates and altered tuffs. Malatya Volcanics and volcano-sedimantary units show gradial transition to Alibonca, and have thick tuff levels, basaltic lavas and cherty limestones. Goal of this study 1-Ascertain of mineralogy and geochemistry of lower and upper levels of marine Alibonca Formation and Malatya lacustrine formation.
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