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Comparison of Major and Trace-Element Enrichments of Pliocene Coal Fields from Karapınar and Ilgın (Konya) Basins (Turkey)
Authors: Mehmet ALTUNSOY, Orhan ÖZÇELİK, C. Bertan GÜLLÜDAĞ
Number of views: 212
In this study, the element contents of two seperate Pliocene aged coal units (from Ilgın and Karapınar coal fields, Konya Basin, Turkey) have been compared. First of these areas, The Karapınar area is east of Konya, and the second area (Ilgın) is west of Konya city (Turkey). Both areas are analyzed for their main and trace element enrichments and compared. In the Karapınar area; pre-Neogene basement rocks comprise Jurassic-Cretaceous units. These units are overlain by Neogene fluvial sediments and lacustrine deposites. Coals are found in the lacustrine sediments. In the Ilgın area; the pre-Neogene rocks are made of Paleozoic-Mesozoic metamorphic rocks and crystalline limestone. Coal bearing sediments lie unconformably on the Mesozoic-Paleozoic rocks. The Pliocene coal bearing units are made of conglomerate, sandstone, siltstone and claystone. When Karapınar coals are compared to the average universal coal content, high element values are found for As, Cs, Ni, Sr, U and V. In the case of Ilgın, Ti, Cs, Rb, Ta, Th, As, Nb, La, Ce, Pr, Nd and Sm are above average. Only As and Cs are the enriched elements in both areas. Lithologic differences of the areas are the cause of the variations of the element enrichments.