Zobrazeno 1 - 10
of 13
pro vyhledávání: '"METE, ÇETİNKAPLAN"'
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:
Mete Çetinkaplan
Publikováno v:
Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey. :92-130
Alanya Masifi’nin dogu kesimde yer alan Anamur bolgesi yuksek sicaklik metamorfizmasi ile tanimlanmaktadir. Bolgede bazik ve asidik meta-magmatikler tarafindan kesilen, ust amfibolit fasiyesi kosullarinda baskalasima ugramis metakirintililar (Saria
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f114faa6f10714c17f43e27a7834229
https://doi.org/10.25288/tjb.358187
https://doi.org/10.25288/tjb.358187
Autor:
Mete Çetinkaplan
Publikováno v:
Volume: 29, Issue: 7 1073-1099
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
Metamorphic evolution of an epidote-lawsonite blueschist sample characterized by the coexistence of lawsonite and epidote from Sivrihisar area (Taysanli Zone) was studied herein in terms of petrology and mineral equilibria. Based on the textural evid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c6f1062e3d0d9edfd05204f4832acab
https://dergipark.org.tr/tr/pub/tbtkearth/issue/62428/942319
https://dergipark.org.tr/tr/pub/tbtkearth/issue/62428/942319
Autor:
Osman Candan, Fırat Şengün, Mete Çetinkaplan, Aral I. Okay, O. Ersin Koralay, Hüseyin Kozlu, Amaury Pourteau, Fukun Chen, Roland Oberhänsli
The Alanya Massif, which is located to the south of central Taurides in Turkey, presents a typical nappe pile consisting of thrust sheets with contrasting metamorphic histories. In two thrust sheets, Sugozu and GundogmuAY nappes, HP metamorphism unde
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3d72a9bd6cb7975ee100bf6f5fc52595
https://avesis.deu.edu.tr/publication/details/53044c53-309b-4922-a2ed-581742a4ae96/oai
https://avesis.deu.edu.tr/publication/details/53044c53-309b-4922-a2ed-581742a4ae96/oai
Autor:
Friederike C. Warkus, Osman Candan, Roland Oberhänsli, S. Dürr, Mete Çetinkaplan, Julius Partzsch, O. Özcan Dora
Publikováno v:
International Journal of Earth Sciences. 89:793-811
The Menderes Massif is made up of Pan-African basement and a Paleozoic to Early Tertiary cover sequence imbricated by Late Alpine deformation. The Precambrian basement comprises primarily medium- to high-grade schists, paragneisses, migmatites, ortho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d0561c5d30d9d8dac66cd077a833b5e
https://doi.org/10.1007/s005310000097
https://doi.org/10.1007/s005310000097
Autor:
METE, ÇETİNKAPLAN, AKAL, CÜNEYT, CANDAN, OSMAN, ROLAND, OBERHAENSLI, KORALAY, OSMAN ERSİN, POURTEAU, AMAURY
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2605::ddfc82b906072f647215aceabad3263d
https://avesis.deu.edu.tr/publication/details/61d3e9f3-1913-4925-a0cb-15b41f9686b5/oai
https://avesis.deu.edu.tr/publication/details/61d3e9f3-1913-4925-a0cb-15b41f9686b5/oai
The Cretaceous blueschist belt, Tavsanli Zone, representing the subducted and exhumed northern continental margin of the Anatolide-Tauride platform is exposed in Western Anatolia. The Sivihisar area east of Tavsanli is made Lip of tectonic units cons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::261d344efdf3bea0803e562787df475e
https://avesis.deu.edu.tr/publication/details/c5a7257d-f988-4774-916e-90a64a3a8aa2/oai
https://avesis.deu.edu.tr/publication/details/c5a7257d-f988-4774-916e-90a64a3a8aa2/oai
Carpholite+chloritoid+pyrophyllite association occurs widely in the Triassic metaclastic rocks of the Afyon Zone in west-central Turkey. Fe-Mg-carpholite is associated with rare aragonite pseudomorphs and glaucophane in marbles and metabasites, respe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cc292168897f6307d6bb165c37524b0d
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/13545
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/13545
Autor:
Mete Çetinkaplan, Gaëtan Rimmelé, Roland Oberhänsli, Osman Candan, Bruno Goffé, Laurent Jolivet
Publikováno v:
Lithos
Lithos, Elsevier, 2003, 71, pp.19-46. ⟨10.1016/S0024-4937(03)00089-6⟩
Lithos, 2003, 71, pp.19-46. ⟨10.1016/S0024-4937(03)00089-6⟩
Lithos, Elsevier, 2003, 71, pp.19-46. ⟨10.1016/S0024-4937(03)00089-6⟩
Lithos, 2003, 71, pp.19-46. ⟨10.1016/S0024-4937(03)00089-6⟩
The Menderes Massif occupies a large part of western Turkey. It is tectonically overlain by nappes of the Izmir-Ankara Suture Zone (including the Bomova Flysch Zone) on its northern flank, the Afyon Zone on its eastern border, and the Lycian Nappes o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::745cb3ed3ec2cc01bf35d592873a3cfb
https://hal.archives-ouvertes.fr/hal-00022373
https://hal.archives-ouvertes.fr/hal-00022373