%0 Journal Article
%T The Stratigraphy between of the Ayd£¿nc£¿k and Duruhan
%A Ahmet Turan
%J -
%D 2019
%X The allochthonous unit, known as Alada£¿ Unit or Hadim Nappe is around Ayd£¿nc£¿k. In the area, the stratigraphic sequence starts by Asarl£¿kyaylas£¿ formation with Upper Devonian which made up of dolomit with macrofossil limestone, quartzite and shale. The Upper Devonian sequences are covered by Carboniferous aged Yar£¿cak formation, containing alternation of fossilliferous limestone and quartzite. With Girvenella, crinoid and fusulin limestones are the representativies of the Arpal£¿k Formation. It underlies Yar£¿cak formation conformably, overlied by Late Permian Ku£¿akda£¿£¿ formation disconformably. The Kusakda£¿£¿ formation starts with shale-quartzite intercalation and continues with algae limestones. Early Triassic G£¿k£¿epinar formation is made up of oolitic-stratmatolithic limestone. At the top, the G£¿k£¿ep£¿nar formation shows transition to Early-Middle Triassic G£¿zta£¿£¿ formation with shales, marls and with bivalve limestone. Lias-Dogger terrestrial £¿ami£¿i formation is made of red conglomerate-sandstone-mudstone, which is covered by Dogger-Malm Dedebeleni formation including varius colors of mudstone, shale, limestone with semi-terrestrial character. Stratigraphic sequence continues with Malm-Cretaceous Cihandere formation, which is made up of dolomite and limestone. The Cihandere formation was covered by the Hasanc£¿k formation as conformable, is represented by pelagics. In the Ayd£¿nc£¿k area the whole sequences were covered by the Burdigalian Mut formation as unconformable, is represented by neritic carbonates
%K Alada£¿ Birli£¿i
%K Hadim nap£¿
%K Devoniyen-Kretase istifleri
%U http://dergipark.org.tr/deumffmd/issue/44128/468966