Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Erhan AKAY"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 142, Iss 142, Pp 165-190 (2011)
Menderes Masifi' nin çok geniş bölümlerinde yüzeyleyen gnaysik granitlerin yerleşim yaşları ve mekanizmalarının belirlenmesi, masifin tektonik evriminin anlaşılması açısından kritik önem taşır. Birçok araştırıcı bu gnayslardan
Externí odkaz:
https://doaj.org/article/f2daf431b9a745ce905bd973920a6e8d
Publikováno v:
Journal of Geodynamics. 50:67-80
The northern border of the Menderes Massif is dominated by gneiss-schist-marble association and meta- granites. The high-grade units of the massif are tectonically overlain by a meta-platform sequence of the Afyon Zone and the Cretaceous-early Tertia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0585de6f23b202d9e440d93f578f3f7d
https://doi.org/10.1016/j.jog.2010.03.002
https://doi.org/10.1016/j.jog.2010.03.002
Autor:
Erhan Akay, Burhan Erdoğan
Publikováno v:
Journal of Asian Earth Sciences. 24:367-387
In the Foca Region, a complete Miocene volcano-sedimentary succession outcrops. This succession includes a well-developed central volcano gradually interdigitating with flank erruptions and a lacustrine sedimentary succession. The Dumanhdag volcano c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::64b9379e67d33162597f131010f97bdf
https://doi.org/10.1016/j.jseaes.2004.01.015
https://doi.org/10.1016/j.jseaes.2004.01.015
Autor:
ERDOĞAN, Erhan Akay &, AKGÜN, Funda
Publikováno v:
Volume: 11, Issue: 2 127-160
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
In central Turkey the Çankırı Basin developed between the Kırşehir and Sakarya continents as a collisional basin during the Tertiary. Along the southern border, between Yozgat and Yerköy, the basin fill predominantly comprises continental and s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=tubitakulakb::4ea9dcbcd52ae0326d0fd52b0648aad5
https://dergipark.org.tr/tr/pub/tbtkearth/issue/12026/143796
https://dergipark.org.tr/tr/pub/tbtkearth/issue/12026/143796
The Kazda Massif was previously considered as the metamorphic basement of the Sakarya Zone, a microcontinental fragment in NW Anatolia. Our new field mapping, geochemical investigations, and radiometric dating lead to a re-evaluation of previous sugg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6bc85024f470dac01c1e4414aa43787c
https://avesis.deu.edu.tr/publication/details/7e9376ca-c89a-4ba2-a89a-e351a11a3436/oai
https://avesis.deu.edu.tr/publication/details/7e9376ca-c89a-4ba2-a89a-e351a11a3436/oai
During the Alpine orogeny, the northern margin of the Tauride-Anatolide Block was deeply buried below the Sakarya continent and subjected to high pressure/low temperature metamorphism. Along this suture zone Tavsanli Zone, Afyon Zone, Bornova Flysch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7d718c9c24ac720d3090ed2b8ca6479b
https://avesis.deu.edu.tr/publication/details/609cf8a2-2035-4db6-9ba4-f5890ed1d052/oai
https://avesis.deu.edu.tr/publication/details/609cf8a2-2035-4db6-9ba4-f5890ed1d052/oai
The Alacam region of NW Turkey lies within the Alpine collision zone between the Sakarya continent and the Menderes platform. Four different tectonic zones of these two continents form imbricated nappe packages (including the Afyon zone), intruded by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eabbb90f409d746a2f28e87ed99b6c77
https://aperta.ulakbim.gov.tr/record/19733
https://aperta.ulakbim.gov.tr/record/19733
Autor:
Erhan Akay
The Oligo-Miocene granitic plutons and their related volcanic-subvolcanic successions form a NW-SE trending magmatic belt along the northern border of the Menderes Massif. This belt evolved within a nappe package consisting of the Menderes metamorphi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cae13f048705b1a6cc010476c657cd42
https://avesis.deu.edu.tr/publication/details/1f0ccc23-f001-4af9-b9d4-3023e2a55113/oai
https://avesis.deu.edu.tr/publication/details/1f0ccc23-f001-4af9-b9d4-3023e2a55113/oai
Autor:
Erhan Akay, Burhan Erdoğan
In western Anatolia, a thick volcanic succession of andesitic to rhyolitic lavas and volcaniclastic rocks crops out extensively. On Foca Peninsula, the westernmost part of the region, a dominantly rhyolitic sequence is exposed where massive rhyolites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1b6e28b4ac500517ef0ab39a155f30c2
https://avesis.deu.edu.tr/publication/details/66f11cad-90a7-45ea-be67-a0750f17b532/oai
https://avesis.deu.edu.tr/publication/details/66f11cad-90a7-45ea-be67-a0750f17b532/oai
The Cankiri Basin evolved as a detrital basin during the Late Tertiary in Central Anatolia between the Pontides (Sakarya continent) and the Kirsehir block. It is E-W trending, and along its southern border it overlies the Kirsehir block unconformably
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2df6c52f647e9a5b1ed130bf1eda3b43
https://avesis.deu.edu.tr/publication/details/20f27e81-61ab-4cda-af5f-49d81943445d/oai
https://avesis.deu.edu.tr/publication/details/20f27e81-61ab-4cda-af5f-49d81943445d/oai