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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... -
(Figure 3) Hematite and Goethite in Luochuan samples
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(Figure 2) Hematite and Goethite in Ganzi_loess_section samples
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Results of bulk sediment X-ray diffraction analysis and quantification of min...
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(Table 2) Whole-rocke geochemistry of lava units at DSDP Holes 55-433C and 55...
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(Table 3) Occurrence of secondary minerals in in veins and vesicles of basalt...
Sediment depth is given in mbsf. P = present; ? = uncertanty. -
(Table 11) Fe-Ti oxide geothermometry at DSDP Holes 73-519A and 73-524
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(Table 5) Major elements in different minerals at DSDP Hole 84-567A
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(Table 1) Major elements at DSDP Hole 89-462A
Fe2O3 and FeO, Mg numbers, and CIPW norms calculated using Fe2O3/FeO ratio of 0.15. -
(Table 1) Heavy fraction minerals in bottom sediments of the Markov Deep, Mid...
An additional ore field in the central part of the MARhas been discovered. Together with previously discovered Logachev (14°45'N) and Ashadze (12°58'N) ore fields, the new ore... -
(Table 5) Composition of heavy minerals in marine sandy loams from the Shapki...
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(Table 4) Composition of heavy minerals in fluvioglacial sediments from the S...
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(Table 3) Composition of heavy minerals in sediments of the Rodionov Horizon ...
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(Table 14-2) Normative mineral composition of epibasalts from the Romanche Fr...
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