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XRD mineralogical abundances in sediments off Milos, Greece
Mineralogical abundances from XRD reported as weight percent (values normalized to 1 = 100%). -
Abundance of minerals in the rocks of the lower peak ring from IODP Hole 364-...
This dataset has no description
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(Table 1) Chemical composition and CIPW norms of basalts at DSDP Site 61-462
Analyst: H. Haramura. -
(Table 3) Major element contents and minerals at DSDP Legs 69-70 Holes
Normative magnetite (mt), which was always a value of 2.18 because Fe2O3 was fixed at a value of 1.5% for the normal calculations, was omitted from the table. -
(Table 3) Modal analyses of secondary minerals in weathered and hydrothermal ...
This dataset has no description
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(Table 2) Chemical composition of complexly zoned plagioclases from DSDP Hole...
This dataset has no description
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(Table 2) Chemical composition of complexly zoned plagioclases from DSDP Hole...
This dataset has no description
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(Table 1) Chemical composition of simply zoned plagioclases from DSDP Site 45...
This dataset has no description
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(Table 2) Geochemistry of K-feldspars and associated plagioclase phenocrysts ...
Basalts from some holes of the Deep Sea Drilling Project contain secondary K-feldspar which forms pseudomorphs after calcic (>76% An) Plagioclase cores, whereas Plagioclase... -
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 T13) Geochemical composition of plagioclase microliths, phenocrysts, a...
This dataset has no description
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(Table 2) Component assemblages in turbiditic sequences at ODP Site 108-657
Abundance: TA = very abundant (>50%), A = abundant (25-50%), P = present (10-25%), R = rare (5% or <5%), - = no grains. -
(Table 3.1.8) Mineral composition of surface layer bottom sediments from the ...
0 = not found; <1 = traces.
