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Clay mineralogy of sdiment core PS2163-1 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 PS2162-1 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 PS2161-1 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 PS2160-3 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 PS2159-3 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 PS2158-1 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 PS2157-3 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...
