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XRD mineralogy of sediment core PS2641-4
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core PS2640-6
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core PS2631-5
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core PS2630-5
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core PS2629-2
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core PS2627-5
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core PS2623-4
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
XRD mineralogy of sediment core JM07-WP-174-GC
We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are... -
(Table A1) Microprobe analysis of plagioclase around fluid inclusions in Grub...
This dataset has no description
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Table D.11: Microprobe analysis of plagioclase and K-feldspar from sample 2119
Number of ions on the basis of 8 O; oxides given in weight percentage -
Table D.10: Microprobe analysis of feldspars from sample 2118
Number of ions on the basis of 8 O; oxides given in weight percentage -
(Table 5) Geochemistry of glasses in pyroxenes and plagioclases at DSDP Sampl...
Empty cells = no data. -
(Table 1) Chemical composition of plagioclase from DSDP Hole 89-462A
This dataset has no description
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(Table 7) Major-element compositions of selected secondary minerals: albite, ...
This dataset has no description
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(Table 3) Analyses of plagioclase and its alteration products of ODP Hole 123...
This dataset has no description
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(Table 9) Chemical composition of whole rocks from DSDP sites
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 8) Chemical composition of whole rocks from ODP Hole 121-758A
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 7) Chemical composition of whole rocks from ODP Site 121-757B
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 6) Chemical composition of whole rocks from ODP Site 121-756
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 3) Chemical composition of feldspars of basalts from ODP Leg 121
This dataset has no description
