Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys

Cüneyt AKAL, (Dokuz Eylül Üniversitesi, Jeoloji Mühendisliği Bölümü, İzmir, Türkiye)
O. Ersin KORALAY, (Dokuz Eylül Üniversitesi, Jeoloji Mühendisliği Bölümü, İzmir, Türkiye)
Osman CANDAN, (Dokuz Eylül Üniversitesi, Jeoloji Mühendisliği Bölümü, İzmir, Türkiye)
Roland OBERHANSLI, (Institut für Erd und Umweltwissenschat en, Univ. Potsdam, Karl Liebknecht Strasse 24, Potsdam 14476, Germany)
Fukun CHEN (Chinese Academy of Sciences Key Laboratory of Crust Mantle Material and Environment, Univ. of Science and Technology of China, Hefei 230026, China)
Turkish Journal of Earth Sciences
2 0
Yıl: 2011 Cilt: 20 Sayı: 3 Sayfa Aralığı: 255 - 271 Metin Dili: Türkçe İndeks Tarihi: 29-07-2022

Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys

Öz:
Türkiye’nin Anatolid-Torid Bloğu’nun bir parçası olarak nitelendirilen Karaburun Yarımadası, Gondvana’nınkuzey kenarında çökelmiş kırıntılı ve karbonatlara ait serileri içermektedir. Erken Triyas yaşlı granitoid tarafından kesilenve Mezosoyik melanj istii ni tektonik olarak üzerleyen Paleozoyik kırıntılı seri üç alt üniteye ayrılabilir: kumtaşı-şeylardalanmasından oluşan alt kırıntılı alt-ünite, siyah çört içerikli şeyl ile kumtaşı ve konglomeradan oluşan üst kırıntılıalt-ünitesi ve Permo–Karbonifer karbonat alt-ünite. Erken Triyas yaşlı I-tipi Karaburun granitoidi, yüksek ilksel$^ {87}Sr/^ {86} Sr$ oranına (0.709021–0.709168), düşük ilksel$^ {143} Nd/^ {144} Nd$ oranına (0.512004–0.512023) ve εNd (–5.34 ile –5.70) izotopikdeğerine sahiptir. Jeokronolojik veriler granitoidin kristalizasyon (sokulum) yaşını 247.1±2.0 my (Sikitiyen) olduğunubelirtmektedir. Bu asidik magmatizma dalma-batma ile ilişkili kıtasal-yay tektonik ortam koşullarının yansıtmaktadır.Söz konusu tektonik ortam, Paleo-Tetis Okyanusu’nun güneye doğru, Gondwana altına dalması-batması sırasındaGondwana’nın kuzey kenarı boyunca gelişen kıtasal yay-arkası yırtılma ile ilişkili Neo-Tetis okyanusunun kuzeykolunun açılması şeklinde yorumlanabilir.
Anahtar Kelime:

Konular: Jeoloji

Neo-Tetis’in gelişim tarihi içinde erken triyas Karaburun granitoidi’nin (Batı Türkiye) jeodinamik Önemi

Öz:
The Karaburun Peninsula, which is considered part of the Anatolide-Tauride Block of Turkey, contains clasticand carbonate sequences deposited on the northern margin of Gondwana. The Palaeozoic clastic sequence, which isintruded by the Early Triassic granitoid and tectonically overlies a Mesozoic mélange sequence, can be divided into threesubunits: a lowerclastic subunit consisting of a sandstone-shale alternation, an upper clastic subunit consisting of blackchert-bearing shales, sandstone and conglomerate, and a Permo–Carboniferous carbonate subunit. h e lower TriassicKaraburun I-type granitoid has a high initial$^ {87}Sr/^ {86} Sr$ ratio (0.709021–0.709168), and low$^ {143} Nd/^ {144} Nd$ ratio (0.512004– 0.512023) and εNd (–5.34 to –5.70) isotopic values. Geochronological data indicate a crystallization (intrusion) ageof 247.1±2.0 Ma (Scythian). Geochemically, the acidic magmatism rel ects a subduction-related continental-arc basintectonic setting, which can be linked to the opening of the northern branch of Neo-Tethys as a continental back-arcrit ing basin on the northern margin of Gondwana. h is can be related to the closure through southward subduction ofthe Palaeotethys Ocean beneath Gondwana.
Anahtar Kelime:

Konular: Jeoloji
Belge Türü: Makale Makale Türü: Araştırma Makalesi Erişim Türü: Erişime Açık
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APA AKAL C, KORALAY O, CANDAN O, OBERHANSLI R, CHEN F (2011). Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. , 255 - 271.
Chicago AKAL Cüneyt,KORALAY O. Ersin,CANDAN Osman,OBERHANSLI Roland,CHEN Fukun Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. (2011): 255 - 271.
MLA AKAL Cüneyt,KORALAY O. Ersin,CANDAN Osman,OBERHANSLI Roland,CHEN Fukun Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. , 2011, ss.255 - 271.
AMA AKAL C,KORALAY O,CANDAN O,OBERHANSLI R,CHEN F Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. . 2011; 255 - 271.
Vancouver AKAL C,KORALAY O,CANDAN O,OBERHANSLI R,CHEN F Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. . 2011; 255 - 271.
IEEE AKAL C,KORALAY O,CANDAN O,OBERHANSLI R,CHEN F "Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys." , ss.255 - 271, 2011.
ISNAD AKAL, Cüneyt vd. "Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys". (2011), 255-271.
APA AKAL C, KORALAY O, CANDAN O, OBERHANSLI R, CHEN F (2011). Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. Turkish Journal of Earth Sciences, 20(3), 255 - 271.
Chicago AKAL Cüneyt,KORALAY O. Ersin,CANDAN Osman,OBERHANSLI Roland,CHEN Fukun Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. Turkish Journal of Earth Sciences 20, no.3 (2011): 255 - 271.
MLA AKAL Cüneyt,KORALAY O. Ersin,CANDAN Osman,OBERHANSLI Roland,CHEN Fukun Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. Turkish Journal of Earth Sciences, vol.20, no.3, 2011, ss.255 - 271.
AMA AKAL C,KORALAY O,CANDAN O,OBERHANSLI R,CHEN F Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. Turkish Journal of Earth Sciences. 2011; 20(3): 255 - 271.
Vancouver AKAL C,KORALAY O,CANDAN O,OBERHANSLI R,CHEN F Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys. Turkish Journal of Earth Sciences. 2011; 20(3): 255 - 271.
IEEE AKAL C,KORALAY O,CANDAN O,OBERHANSLI R,CHEN F "Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys." Turkish Journal of Earth Sciences, 20, ss.255 - 271, 2011.
ISNAD AKAL, Cüneyt vd. "Geodynamic significance of the early triassic Karaburun granitoid (Western Turkey) for the opening history of Neo-Tethys". Turkish Journal of Earth Sciences 20/3 (2011), 255-271.
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