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This page is a summary of: Al2O3/TiO2 ratio of the clay fraction of Late Ordovician–Silurian carbonate rocks as an indicator of paleoclimate of the Fennoscandian Shield, Palaeogeography Palaeoclimatology Palaeoecology, December 2012, Elsevier,
DOI: 10.1016/j.palaeo.2012.10.001.
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