Zobrazeno 1 - 10
of 17
pro vyhledávání: '"O. Özcan DORA"'
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:
O. Özcan DORA
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 142, Iss 142, Pp 1-23 (2011)
Menderes Masifinin Pan-Afrikan temeli, paragnays ve onu üzerleyen şist birimlerinden yapılı monoton metakırıntılı serisi ve bunları kesen metagabro ve farklı türde gnays ve metagranitlerden yapılıdır. Temeli, kuvarsit ve metaçakıltaş
Externí odkaz:
https://doaj.org/article/ec9223809cde4cc48453e5ad4f4efa76
Autor:
O. Ersin KORALAY, Osman CANDAN, Cüneyt AKAL, O. Özcan DORA, Fukun CHEN, Muharrem SATIR, Roland OBERHÄNSLI
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 142, Iss 142, Pp 69-119 (2011)
Menderes Masifi (MM), Türkiye'nin batısında Alpin Orojenik Kuşağı içerisinde geniş alanda yüzeyleyen metamorfik bir komplekstir. Masif ana olarak, Prekambriyen yaşlı bir temel ve onu üzerleyen Paleozoyik-Erken Tersiyer yaşlı örtü seri
Externí odkaz:
https://doaj.org/article/004a48aeae7f4501a8db36d34c28c0b9
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:
O. Özcan Dora, O. E. Koralay, Muharrem Satir, Osman Candan, Cüneyt Akal, Roland Oberhänsli, Fukun Chen
Publikováno v:
International Journal of Earth Sciences. 101:2055-2081
The Menderes Massif, exposed in western Anatolia, is a metamorphic complex cropping out in the Alpine orogenic belt. The metamorphic rock succession of the Massif is made up of a Precambrian basement and overlying Paleozoic-early Tertiary cover serie
Publikováno v:
Volume: 15, Issue: 3 321-342
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
The Menderes Massif, which covers a large area in western Turkey, is made up of Pan-African basement rocks and a Palaeozoic to Early Tertiary cover sequence. The study area is located in the Dalama and Hallaçlar (Aydın) area, in the northern and ce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=tubitakulakb::f1d7266f86f2828ceddcf4a69875d33f
https://dergipark.org.tr/tr/pub/tbtkearth/issue/12013/143729
https://dergipark.org.tr/tr/pub/tbtkearth/issue/12013/143729
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
Publikováno v:
International Journal of Earth Sciences. 89:836-851
The Pan-African basement of the Menderes Massif comprises a regular lithological succession that reaches a thickness of 8 km, the oldest units of which are, in ascending order, so-called leptite-gneisses, a quartzite-sequence transition zone and mica
Autor:
Osman Candan, Orhan Kaya, Cüneyt Akal, O. Özcan Dora, N. Konak, O. E. Koralay, Roland Oberhänsli, Fukun Chen
Well-preserved primary contact relationships between a Late Proterozoic metasedimentary and the metagranitic core and Palaeozoic cover series of the Menderes Massif have been recognized in the eastern part of the Cine submassif on a regional-scale. M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6dcc0aae3c70fe9236d6c8eba2524ddb
https://aperta.ulakbim.gov.tr/record/18591
https://aperta.ulakbim.gov.tr/record/18591
Metagabbros in the core series of the Menderes Massif, for some time considered as post orogenic Miocene intrusives, revealed a strong poly-metamorphic history. The metagabbro bodies exhibit a pronounced zonation. Within their cores, igneous minerals
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::86609cbae179dda43969162275470406
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/24674
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/24674