Çayeli (Rize) ve İspir (Erzurum) arasında kalan alanın tektonostratigrafik özellikleri

Autor: İsmet ALAN, Veli BALCI, Halil KESKİN, İbrahim ALTUN, Nevzat BÖKE, Hünkar DEMİRBAĞ, Sedat ARMAN, Hasan ELİBOL, Mustafa SOYAKİL, Alican Kop, Nurullah HANİLÇİ

Publikováno v: Bulletin of the Mineral Research and Exploration, Vol 158, Iss 158, Pp 1-29 (2019)

İnceleme alanı Doğu Pontidler’de Rize, Çayeli, Arhavi, İspir İkizdere arasında kalan alanı kapsamaktadır. Bu alanda Maçka Tektonik Dilimi (MTD) ve Taşköprü Tektonik Dilimi (TTD) yüzeylenmektedir. MTD yaşlıdan gence doğru; Geç Jura

Externí odkaz: https://doaj.org/article/51ce7d333761444c90607b41fa6de9be

Tectonostratigraphic characteristics of the area between Çayeli (Rize) and İspir (Erzurum)

Autor: Mustafa Soyakil, Hasan Elibol, Alican Kop, Sedat Arman, Veli Balci, Halil Keskin, İbrahim Altun, Nevzat Böke, Hünkar Demirbağ, İsmet Alan, Nurullah Hanilçi

Publikováno v: Volume: 158, Issue: 158 1-29
Bulletin of the Mineral Research and Exploration

The study area is located in the Eastern Pontides between Rize, Çayeli, Arhavi, İspir and İkizdere. In this area, Maçka Tectonic Slice (MTS) and Taşköprü Tectonic Slice (TTS) are exposed. MTS is composed from old to young; Late Jurassic-Early

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8601a339adc2a8b1424ea7c6cd7cd58c
https://hdl.handle.net/20.500.12831/6804

Alkaline series related to Early-Middle Miocene intra-continental rifting in a collision zone: An example from Polath, Central Anatolia, Turkey

Autor: Hünkar Demirbağ, Pınar Alıcı, Hervé Bellon, Abidin Temel, Tekin Yürür, Alain Gourgaud, Elif Varol

Publikováno v: Journal of Southeast Asian earth sciences
Journal of Southeast Asian earth sciences, 2010, 29, pp.289-306. ⟨10.1016/j.jseaes.2009.12.017⟩
Journal of Southeast Asian earth sciences, Elsevier, 2010, 29, pp.289-306. ⟨10.1016/j.jseaes.2009.12.017⟩

A large volcanic area (∼7600 km2), the Galatean Volcanic Province (GVP), developed in northwest Central Anatolia during the Miocene along the Neo-Tethys Ocean suture zone possibly by post-collisional processes. The GVP mainly comprises 20–14 My o

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3fbff1513dd540d1ff2a69dd0ef0e9de
https://hal.science/hal-00523360