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Clay mineral composition of sediments from the Prydz Bay-Kerguelen region
This dataset has no description
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(Table 2) Sulfur and organic carbon values and clay minerals from the Caravac...
Distance refers to 80 cm thick interval spanning the K/T boundary at Caravaca (-40 to + 40 cm in which the base of the fallout lamina is defined as 0 cm; positive and negative... -
(Table 2) Sedimentology and clay mineral content of surfac sediments from the...
of carbonate-free fraction, clay < 2 µm -
Figure 2. Sedimentology of core PS2185-6
This dataset has no description
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Clay mineral composition of sediment core GeoTü SL112
This dataset has no description
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(Supp. Fig.) Clay mineral content of sediment core PS2540-3
This dataset has no description
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(Fig. 3i) Clay mineral content of sediment core PS2538-2
This dataset has no description
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(Fig. 3e) Clay mineral content of sediment core PS2533-2
This dataset has no description
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(Fig. 2) Clay mineral composition of seabed surface sediments
This dataset has no description
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(Table 3) Abundance of clay minerals of Hole 302-M0002A
This dataset has no description
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Relative mineral abundances from bulk fraction X-ray diffraction data of Hole...
This dataset has no description
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Sedimentology on core PS58/254-1
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...
