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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 2) Major element analyses of representative Leg 91 basalts
CIPW norms calculated with assumed Fe2O3/Fe= ratio of 0.15. -
XRD mineralogy of sediments from the Greenland east coast
Quantitative X-Ray Diffraction (qXRD) analysis of the <2 mm sediment fraction from surface (sea floor) samples, and marine sediment cores that span the last 10-12 cal ka BP,... -
Smear slide analysis of Hole 25-248
This dataset has no description
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Bulk mineralogy of sediment core AMD0214-02PC and HLY0501-05JPC from the west...
This dataset has no description
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(Table 4.1) Mineral composition of Mariana back-arc sediment cores
This dataset has no description
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Quantitative X-ray diffraction replicate results of the weight % of non-clay ...
This dataset has no description
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(Table 4) Geochemistry and minerals of diabase at DSDP Holes 63-469 and 63-471
The norms were calculated after Fe2O3 was reduced to FeO so as to have Fe2O3/FeO = 0.25. -
(Table 6) Major element compositions and norms of basalts at DSDP Leg 63 Holes
The norms were calculated after Fe2O3 was reduced to FeO so as to have Fe2O3/FeO = 0.25. -
(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) Geochemistry of DSDP Hole 65-485A basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
(Table 6) Geochemistry of DSDP Hole 65-483B basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15. -
(Table 5) Geochemistry of DSDP Hole 65-483 basalts
CIPW norms determined assuming an Fe2O3/FeO ratio of 0.15.