Abstract
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.
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Acknowledgments
We would like to thank the two reviewers Mete Çetinkaplan and Donna Whitney for all comments that helped to improve this manuscript. Furthermore, we thank the anonymous reviewer for his/her stimulating comments that helped to make the discussion more clear. All staff members of Potsdam University, RUB and GFZ are thanked for everyday’s engagement, laboratory assistance and fruitful discussions: Christine Fischer, Christina Günter, Martin Ziemann, Antje Musiol, Anja Städtke, Rolf Neuser, Dieter Rhede. Philipp Balling was a helpful assistant in ArcGIS. This project is funded by the DFG (Deutsche Forschungsgemeinschaf; Project Number: OB 80/51-1).
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Scheffler, F., Oberhänsli, R., Pourteau, A. et al. Sedimentologic to metamorphic processes recorded in the high-pressure/low-temperature Mesozoic Rosetta Marble of Anatolia. Int J Earth Sci (Geol Rundsch) 105, 225–246 (2016). https://doi.org/10.1007/s00531-015-1214-y
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DOI: https://doi.org/10.1007/s00531-015-1214-y