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(Table 1) Age and lithological description of sediment core MD99-2227
For bulk mineralogy, semiquantitative estimation was obtained by applying correction factors to the measured intensity of the reflections as follows: I3.34 Å * 1 for quartz,... -
(Table 2) Mean values calculated for individual stages and for all the interg...
Clay flux: Normalized flux, i.e., measured clay flux divided by the present flux measured in surface sediment 90-013-017 sample -
(Table 2) Mineralogy at DSDP Hole 86-576A sediments
This dataset has no description
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Distribution of clay minerals in surface sediments of the Eurasian Arctic Ocean
Clay-mineral distributions in the Arctic Ocean and the adjacent Eurasian shelf areas are discussed to identify source areas and transport pathways of terrigenous material in the... -
Tab 7d, Clay mineral distribution of sediment core SO82_7-2
first 37 cm of core occurs twice, core analysis combins GKG and KAL -
Tab 7c, Clay mineral distribution of sediment core SO82_5-2
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Tab 7b, Clay mineral distribution of sediment core SO82_4-2
This dataset has no description
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Tab 7a, Clay mineral distribution of sediment core SO82_2-2
This dataset has no description
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Tab 7f, Clay mineral distribution of sediment core LO09/23-2
This dataset has no description
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Tab 7e, Clay mineral distribution of sediment core LO09/21-2
This dataset has no description
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Tab 5, Grain size and clay mineral distribution of surface sediments from the...
This dataset has no description
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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...
