Kivrim, Drenaj ve Bindirme Morfolojilerine rnekler

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Kivrim, Drenaj ve BindirmeMorfolojilerineÖrnekle
r

• A. M. Celal Sengör ve Umut B. Ülgen

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• Zagrosta cephe kivrimlari bölgesinde yeni açiga
  çikmis bir kivrim üzerinde
• sürempoze drenaj. Sürempozisyon Fars Grubu
  (Orta-Üst Miyosen) üzerinden Asmari
• Formasyonuna (Orta Oligosen-Alt Miyosen)
  olmustur. Sagdaki bogaz Zal Suyunun (Ab-i Zal)
• Kialan antiklinalinin Senomaniyen çekirdeginde
  açilmistir. Burada hem transversal hem de
• otojen drenaj çalismaktadir. Zal daha sonra Alt
  fars formasyonu tarafindan hala üzerlenen
• Asmari Kireçtasinin bir kemerini kesmektedir.
  Ileride, Tang,i Fanni ve Tang-i Laylum, Kialan
• antiklinalinin uç kisimlarini kesmektedirler.

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Bindirmeler
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Referanslar

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