Age and geodynamic evolution of the Black Sea Basin: Tectonic evidences of rifting in Crimea

Creative Commons License

HİPPOLYTE J., MUROVSKAYA A., VOLFMAN Y., YEGOROVA T., GİNTOV O., KAYMAKCI N., ...Daha Fazla

MARINE AND PETROLEUM GEOLOGY, cilt.93, ss.298-314, 2018 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 93
  • Basım Tarihi: 2018
  • Doi Numarası: 10.1016/j.marpetgeo.2018.03.009
  • Dergi Adı: MARINE AND PETROLEUM GEOLOGY
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.298-314
  • Anahtar Kelimeler: Fault, Paleostress, Graben, Rifting, Back arc basin, Inversion, Black Sea, Crimea, ARABIA-EURASIA COLLISION, WESTERN GREATER CAUCASUS, CENTRAL PONTIDES, NORTHERN TURKEY, STRUCTURAL DEVELOPMENT, SUBDUCTION-ACCRETION, CENOZOIC EVOLUTION, CENTRAL ANATOLIA, SOUTHERN MARGIN, HISTORY
  • Kocaeli Üniversitesi Adresli: Evet

Özet

The timing and direction of opening of the Black Sea Basin are debated. However, parts of its margins were inverted during Cenozoic and can be studied onshore. The Crimean Mountains are located in the middle of the northern margin of the basin, and at the onshore prolongation of the mid-Black Sea High.