Sedimentologic to metamorphic processes recorded in the high-pressure/low-temperature Mesozoic Rosetta Marble of Anatolia

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• 作者：F. Scheffler ; R. Oberhänsli ; A. Pourteau…
• 关键词：Gypsum ; High ; pressure metamorphism ; Neotethys ; Anatolia
• 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：225-246
• 全文大小：13,147 KB
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• 作者单位：F. Scheffler (1)
  R. Oberhänsli (1)
  A. Pourteau (1)
  A. Immenhauser (2)
  O. Candan (3)
  
  1. Institute of Earth and Environmental Science, University of Potsdam, 14476, Potsdam-Golm, Germany
  2. Institute of Geology, Mineralogy and Geophysics, Ruhr-University Bochum, 44801, Bochum, Germany
  3. Department of Geological Engineering, Dokuz Eylül Üniversitesi, 35160, Bornova, İzmir, 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

Anatolia’s high-pressure metamorphic belts are characterized in part by a Neotethyan stratigraphic succession that includes a mid-Cretaceous hemi-pelagic marble sequence. This unit contains, towards its stratigraphic top, dm-to-m-long radiating calcitic rods forming rosette-like textures. Here, we refer to these features as “Rosetta Marble”. The remarkable textural similarity of non-metamorphic selenite crystals and radiating calcite rods in the Rosetta Marble strongly suggests that these textures represent pseudomorphs after selenites. Metamorphosed hemi-pelagic limestones, dominated by Rosetta selenite pseudomorphs, are alternating with siliceous meta-sediments containing relictic radiolaria tests. This stratigraphic pattern is indicative of transient phases characterized by evaporites precipitated from basinal brines alternating with non-evaporative hemi-pelagic deposition from normal-marine seawater. The regional distribution of Rosetta Marble exposures over 600 km is indicative of basin-scale evaporitic intervals. High-pressure, low-temperature metamorphism of these rocks is witnessed by Sr-rich (up to 3500 ppm), fibrous calcite pseudomorphs after aragonite and isolated aragonite inclusions in quartz. Peak metamorphic conditions of 1.2 GPa and 300–350 °C are attested by high-Si white mica thermobarometry. The Rosetta Marble case example examines the potential to unravel the complete history from deposition to diagenesis and metamorphism of meta-sedimentary rocks.