MIOCENE ALLUVIAL-FAN ALKALINE PLAYA LIGNITE TRONA BEARING DEPOSITS FROM AN INVERTED BASIN IN ANATOLIA - SEDIMENTOLOGY AND TECTONIC CONTROLS ON DEPOSITION

INCI U.

SEDIMENTARY GEOLOGY, cilt.71, ss.73-97, 1991 (SCI-Expanded, Scopus) identifier identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 71
  • Basım Tarihi: 1991
  • Doi Numarası: 10.1016/0037-0738(91)90008-2
  • Dergi Adı: SEDIMENTARY GEOLOGY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.73-97
  • Dokuz Eylül Üniversitesi Adresli: Hayır

Özet

During the Middle through Late Miocene, over 1200 m of clastics, carbonates and evaporites accumulated in the depositional basin situated in northwestern Ankara province of Central Anatolia. Detailed stratigraphic and sedimentological analyses of the exposed sequence exhibits three major facies: (1) lower alluvial, (2) upper alluvial, and (3) lacustrine.