Özet:

The new stratigraphic classification of the important linyite coal area in mining in the Soma mountains in the south of Soma (is: Manisa) has led to a geological study in a scale of 1:25 000. The sub-structure consists of young Paleozoic grapes and the Upper Jura clusters. Alpidic tectogenesis has formed a crushed curved silsile, and this silsile has turned into a mountainous land in the Transition. Approximately from Helvesienden to this place, it has been drawn with initially contributed coal vessels and covered with fluviatile and limnic collapse and increasing nispette from Pliosenden with andezitic pipe and roof sprites. Today’s playoff begins with the young playoff. The main linyte coal vein is due to the formation of many available conditions and also to find a vuku. The main vein was formed in a pre-Neogenic valley, and this valley became a tectonic land of collapse in Miosende.