
Clay mineralogy (fraction <2µm) of samples from Bir Oum Ali area
Samples taken in February and October 2010. Analysis performed at the Institute of Earth Sciences, University of Lausanne, Swizerland, on an ARL Thermo X'tra diffractometer. The... 
(Table 2) Accumulation rates of ODP Site 128798Clay mineral composition of O...
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Clay mineralogy of sdiment core PS21933 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21922 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21911 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21905 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21893 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21875 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21863 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21854 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21843 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21801 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21793 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21784 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21773 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21754 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21742 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21721 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21712 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay... 
Clay mineralogy of sdiment core PS21702 in the Arctic Ocean
Peak areas representing the clay mineral groups are transformed into relative clay mineral percentages by means of Biscaye's factors (1965) using the assumption that the clay...