Tavşanlı Yöresi 'Ofiolit' Sorununun Ana Çizgileri

Çalışma alanı, İzmir-Ankara Kretase jeosonklinalinin güney kenarında yer alır. Yaklaşık WNW gidişli ve düşey Büyük Fay, alanı birbirinden bağımsız oluşmuş kaya topluluklarını kapsayan iki kesime ayırır.

Anahtar Kelimeler:

Ofiolit, Tavşanlı, Kretase

The studied area is located at the southern boundary of the İzmir-Ankara geosyncline, to the west of Kütahya. The maparea of Budağan Dağ is cut into two segments by an WNW trending steep fault, the Great Fault (new name). On the opposite sides of the Great Fault the rock assemblages are different and the stratigraphie sequences are formed independently.

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