New paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane

ÖKSÜM, Erdinç; Hisarli, Z.; Cinku, Mualla; Ustaomer, Timur; Orbay, Naci

doi:10.1016/j.tecto.2015.08.014

New paleomagnetic results from Ordovician sedimentary rocks from NW Anatolia: Tectonic implications for the paleolatitudinal position of the Istanbul Terrane

Atıf İçin Kopyala

ÖKSÜM E., Hisarli Z. M., Cinku M. C., Ustaomer T., Orbay N.

TECTONOPHYSICS, cilt.664, ss.14-30, 2015 (SCI-Expanded)

Yayın Türü: Makale / Tam Makale
Cilt numarası: 664
Basım Tarihi: 2015
Doi Numarası: 10.1016/j.tecto.2015.08.014
Dergi Adı: TECTONOPHYSICS
Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
Sayfa Sayıları: ss.14-30
İstanbul Üniversitesi Adresli: Evet

Özet

The Istanbul terrane, classically known as the "Paleozoic of Istanbul", is geologically one of the important continental components of NW Turkey. The terrane comprises an Early Ordovician to Early Carboniferous transgressive sedimentary sequence and appears as an exotic unit with respect to its present surroundings.