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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 128-798Clay mineral composition of O...
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Clay mineralogy of sdiment core PS2193-3 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 PS2192-2 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 PS2191-1 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 PS2190-5 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 PS2189-3 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 PS2187-5 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 PS2186-3 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 PS2185-4 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 PS2184-3 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 PS2180-1 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 PS2179-3 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 PS2178-4 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 PS2177-3 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 PS2175-4 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 PS2174-2 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 PS2172-1 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 PS2171-2 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 PS2170-2 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...