A N-S-trending active extensional structure, the Suhut (Afyon) graben: Commencement age of the extensional neotectonic period in the Isparta Angle, SW Turkey


Kocyigit A., Deveci S.

TURKISH JOURNAL OF EARTH SCIENCES, cilt.16, ss.391-416, 2007 (SCI İndekslerine Giren Dergi) identifier

  • Cilt numarası: 16 Konu: 4
  • Basım Tarihi: 2007
  • Dergi Adı: TURKISH JOURNAL OF EARTH SCIENCES
  • Sayfa Sayıları: ss.391-416

Özet

The Suhut graben is an 8 - 11- km- wide, 24- km- long, N - S- trending, active extensional structure located on the southern shoulder of the Aksehir- Afyon graben, near the apex of the outer Isparta Angle. The Suhut graben developed on a pre- Upper Pliocene rock assemblage comprising pre- Jurassic metamorphic rocks, Jurassic - Lower Cretaceous platform carbonates, the Lower Miocene - Middle Pliocene Afyon stratovolcanic complex and a fluvio-lacustrine volcano- sedimentary sequence.