Abstract
Bati Anadoluda bulunan Simav grabeni ve civarinda toplanan gravite verileri, standart sapma suzgeci ve Euler evrisimi kullanilarak yeniden islenmis ve yorumlanmistir. Yorum ve sismolojik calismalarin sonucunda; Simav yakinlarinda sokulum yapilarinin varligi tanimlanmistir. Grabenin dogu kenarinda bulunan ve daha onceki jeofizik calismalarda tanimlanamayan bu sokulumun kalinligi 12-15 km ve yuzeyden derinligi 2.5-3 km dir. Grabenin dogusunda kayit edilen cok sayida deprem bu sokulumla ilintilidir . Simav Grabeni, Simav Fayinin buklumu, Nasa adi verilen Sokulum ve deprem odaklari ayni tektonik karede goruntulenmistir. Gravite verisi iki ve uc boyutlu cozumlenerek bu tektonik ortakligin anlami arastirilmistir. Uc boyutlu model uzerinde tektonik yapilar isaretlenmistir.
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