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Bulk mineral assemblage of sediment core GeoB22336-4, MARIA S. MERIAN cruise ...
This dataset includes mineral assemblages of gravity core GeoB22336-4 retrieved from northern Baffin Bay during cruise MSM66 in 2017. The XRD data were obtained on pulverized... -
Kaolinite/chlorite ratios measured on sediment core PS2564-3
This dataset has no description
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Kaolinite/chlorite ratios measured on sediment core PS2498-1
This dataset has no description
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Kaolinite/chlorite ratios measured on sediment core PS2495-3
This dataset has no description
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Clay mineralogy of sediment core PS2498-1
This dataset has no description
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Clay mineralogy of sediment core PS2495-3
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
This dataset has no description
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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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Sedimentology of core PS2471-4
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...
