P᾿em>T᾿em>t evolution of eclogite/blueschist facies metamorphism in Alanya Massif: time and space relations with HP event in Bitlis Massif, Turkey

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• 作者：Mete Çetinkaplan ; Amaury Pourteau ; Osman Candan…
• 关键词：Tauride ; Eclogite ; Alanya ; Blueschist ; Metamorphism
• 刊名：International Journal of Earth Sciences
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：105
• 期：1
• 页码：247-281
• 全文大小：4,641 KB
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• 作者单位：Mete Çetinkaplan (1)
  Amaury Pourteau (2)
  Osman Candan (1)
  O. Ersin Koralay (1)
  Roland Oberhänsli (2)
  Aral I. Okay (3)
  Fukun Chen (4)
  Hüseyin Kozlu (5)
  Fırat Şengün (6)
  
  1. Department of Geological Engineering, Dokuz Eylül University, 35160, Buca-İzmir, Turkey
  2. Institut für Geowissenschaften, Universitat Potsdam, Postfach 601553, 14415, Potsdam, Germany
  3. Eurasian Institute of Earth Sciences, Technical University of Istanbul, Ayazağa, 80626, Istanbul, Turkey
  4. Chinese Academy of Sciences Key Laboratory of Crust-Mantle Material and Environment, University of Science and Technology of China, Hefei, 230026, China
  5. Turkish Petroleum Corporation (TPAO), Ankara, Turkey
  6. Department of Geological Engineering, Çanakkale Onsekiz Mart University, 17020, Çanakkale, Turkey
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Earth sciences
  Geology
  Geophysics and Geodesy
  
• 出版者：Springer Berlin / Heidelberg
• ISSN：1437-3262

文摘

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, Sugözü and Gündoğmuş nappes, HP metamorphism under eclogite (550–567 °C/14–18 kbar) and blueschist facies (435–480 °C/11–13 kbar) conditions have been recognized, respectively. Whereas the rest of the Massif underwent MP metamorphism under greenschist to amphibolite facies (525–555 °C/6.5–7.5 kbar) conditions. Eclogite facies metamorphism in Sugözü nappe, which consists of homogeneous garnet–glaucophane–phengite schists with eclogite lenses is dated at 84.8 ± 0.8, 84.7 ± 1.5 and 82 ± 3 Ma (Santonian–Campanian) by 40Ar/39Ar phengite, U/Pb zircon and rutile dating methods, respectively. Similarly, phengites in Gündoğmuş nappe representing an accretionary complex yield 82–80 Ma (Campanian) ages for blueschist facies metamorphism. During the exhumation, the retrograde overprint of the HP units under greenschist–amphibolite facies conditions and tectonic juxtaposition with the Barrovian units occurred during Campanian (75–78 Ma). Petrological and geochronological data clearly indicate a similar Late Cretaceous tectonometamorphic evolution for both Alanya (84–75 Ma) and Bitlis (84–72 Ma) Massifs. They form part of a single continental sliver (Alanya–Bitlis microcontinent), which was rifted from the southern part of the Anatolide–Tauride platform. The P–T–t coherence between two Massifs suggests that both Massifs have been derived from the closure of the same ocean (Alanya–Bitlis Ocean) located to the south of the Anatolide–Tauride block by a northward subduction. The boundary separating the autochthonous Tauride platform to the north from both the Alanya and Bitlis Massifs to the south represents a suture zone, the Pamphylian–Alanya–Bitlis suture.