Obduction, subduction and collision as reflected in the Upper Cretaceous-Lower Eocene sedimentary record of western Turkey


Okay A., Tansel I., Tuysuz O.

GEOLOGICAL MAGAZINE, cilt.138, ss.117-142, 2001 (SCI İndekslerine Giren Dergi) identifier identifier

  • Cilt numarası: 138 Konu: 2
  • Basım Tarihi: 2001
  • Doi Numarası: 10.1017/s0016756801005088
  • Dergi Adı: GEOLOGICAL MAGAZINE
  • Sayfa Sayıları: ss.117-142

Özet

Late Cretaceous-Early Eocene Tethyan evolution of western Turkey is characterized by ophiolite obduction, high-pressure/low-temperature metamorphism, subduction, are magmatism and continent-continent collision. The imprints of these events in the Upper Cretaceous-Lower Eocene sedimentary record of western Anatolia are studied in thirty-eight well-described stratigraphic sections. During the Late Cretaceous period, western Turkey consisted of two continents, the Pontides in the north and the Anatolide-Taurides in the south. These continental masses were separated by the Imir-Ankara Neo-Tethyan ocean. During the convergence the Pontides formed the upper plate, the Anatolide-Taurides the lower plate. The are magmatism in the Pontides along the Black Sea coast is biostratigraphically tightly constrained in time between the late Turonian and latest Campanian. Ophiolite obduction over the passive margin of the Anatolide-Tauride Block started in the Santonian soon after the inception of subduction in the Turonian. As a result, large areas of the Anatolide-Tauride Block subsided and became a region of pelagic carbonate sedimentation during the Campanian. The leading margin of the Anatolide-Tauride Block was buried deeply and was deformed and metamorphosed to blueschist facies during Campanian times. The Campanian are volcanic rocks in the Pontides are conformably overlain by shaley limestone of Maastrichtian-Palaeocene age. However, Maastrichtian sedimentary sequences north of the Tethyan suture an of fore-are type suggesting that although are magmatism ceased by the end of the Campanian age, continent-continent collision was delayed until Palaeocene time, when there was a change from marine to continental sedimentation in the fore-are basins. The interval between the end of the are magmatism and continent-continent collision may have been related to a northward jump of the subduction zone at the end of Campanian time, or to continued obduction during the Maastrichtian.