Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Ersin KORALAY"'
Autor:
Osman CANDAN, O. Özcan DORA, Roland OBERHÄNSLI, Ersin KORALAY, Mete ÇETİNKAPLAN, Cüneyt AKAL, Muharrem SATIR, Fukun CHEN, Orhan KAYA
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 142, Iss 142, Pp 25-68 (2011)
Batı Anadolu'da yüzlek veren Menderes Masifi kuzeyde Afyon Zonu, güneyde ise Likya napları tarafından tektonik olarak üzerlenmektedir. Öte yandan kuzeybatıda, Kikladik Kompleks ve onu üzerleyen Likya naplarından yapılı Alpin yaşlı yüks
Externí odkaz:
https://doaj.org/article/e9d14746a11f409483f2a9cac2d87671
Autor:
Osman CANDAN, Roland OBERHÄNSLI, O. Özcan DORA, Mete ÇETİNKAPLAN, Ersin KORALAY, Gaëtan RIMMELÉ, Fukun CHEN, Cüneyt AKAL
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 142, Iss 142, Pp 121-163 (2011)
Batı Anadolu'da yüzlek veren Menderes Masifi ana hatlarıyla Geç Alpin sıkışma tektoniği ile biçimlenmiş karmaşık bir tektonik iç yapı sunmaktadır. Bu kristalin kompleksin litostratigrafik istifi; 1-Pan-Afrikan temel (çekirdek serisi)
Externí odkaz:
https://doaj.org/article/61ae0a72dc474ffe99c49f6bbe6b2cca
Autor:
Halil Yusufoğlu, Meftun Kerem Sönmez, Osman Ersin Koralay, Osman Candan, Muhamed Çoban, Ali Ekber Akçay, Metin Beyazpirinç, Mustafa Kemal Özkan
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 170, Iss 170, Pp 57-85 (2023)
Metamorphites of Niğde Massif, which form the basis of study area covering the Niğde vicinity in Central Anatolia, are composed of Late Devonian Gümüşler, Carboniferous-early Permian Kaleboynu late Permian Kızıldağ formation and unconformable
Externí odkaz:
https://doaj.org/article/b18ab0cf3f3d4f3780a6ab7d4f1b84b0
Autor:
Mustafa Kemal ÖZKAN, Metin BEYAZPİRİNÇ, Ali Ekber AKÇAY, Muhamed ÇOBAN, Osman CANDAN, Osman Ersin KORALAY, Meftun Kerem SÖNMEZ, Halil YUSUFOĞLU
Publikováno v:
Bulletin Of The Mineral Research and Exploration. :1-40
Orta Anadolu’da Niğde dolaylarını kapsayan inceleme alanının temelini oluşturan Niğde Masifi’ne ait metamorfitler alttan üste doğru Geç Devoniyen yaşlı Gümüşler, Karbonifer-erken Permiyen yaşlı Kaleboynu, geç Permiyen yaşlı K
Publikováno v:
Acta Geologica Sinica - English Edition. 95:1199-1216
During the Late Cretaceous in the Eastern Mediterranean, the northern branch of the southern Neotethys was closed by multiple northward subductions. Of these, the most northerly located subduction created the Baskil continental arc at around 82-84 Ma
Publikováno v:
Volume: 29, Issue: 4 617-628
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
The Gonen granitoid is exposed in the western Sakarya Zone and is overlain unconformably by a Jurassic succession. The medium to coarse-grained Gonen granitoid has mineral assemblage of K-feldspar, plagioclase, quartz, muscovite, and biotite. Accesso
Autor:
I. Dogancan Yasar, M. Cemal Göncüoglu, Youn-Joong Jeong, Kaan Sayit, Willis E. Hames, O. Ersin Koralay
The Sakarya Composite Terrane (SCT) in northern Turkey consists of a pre-Jurassic basement composed of several tectonic units. Among these, the Sogut Metamorphics, preserved within the Central Sakarya Terrane (a part of the SCT), is a Variscan tecton
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c0d9a84943c76fa97a2bc2c960f6b934
https://avesis.deu.edu.tr/publication/details/681f2749-8879-4bff-b122-417e5c66dfb5/oai
https://avesis.deu.edu.tr/publication/details/681f2749-8879-4bff-b122-417e5c66dfb5/oai
Autor:
Osman Ersin Koralay, Fatma Nuran Sönmez, Huseyin Yilmaz, Mustafa Çiçek, Jason Kirk, Samuel Niedermann
Publikováno v:
Ore Geology Reviews
The Menderes Massif (MM) is considered to be one of the principal regions hosting vein-type quartz-arsenopyrite orogenic gold deposits and occurrences in Turkey. Gold mineralizations in the MM can be grouped into: (i) schistosity-conformable E-trendi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b179684e5b432f4b2d69df688563f88e
https://aperta.ulakbim.gov.tr/record/3529
https://aperta.ulakbim.gov.tr/record/3529
Autor:
Fırat Şengün, Osman Ersin Koralay
The Jurassic sandstones exposed in the western part of the Sakarya Zone are yellowish to brown, moderate to well sorted, medium to coarse-grained, grain-supported, and cemented by calcareous and minor silica. Sandstones are mainly classified as litha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9cdbad97d1603a83ab4e20a619bb963
https://avesis.deu.edu.tr/publication/details/4d5796a0-37ad-41fd-baee-3a1f6e9da19b/oai
https://avesis.deu.edu.tr/publication/details/4d5796a0-37ad-41fd-baee-3a1f6e9da19b/oai