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Crystallization conditions and compositions of residual melts from the Mid At...
This dataset has no description
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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 C.13: Microprobe analysis of K-feldspar from samples no. 2168 and 2169,...
Number of ions on the basis of 8 O, oxides given in weight percentage -
Table C.10+11+12: Microprobe analysis of plagioclase and K-feldspar from samp...
Number of ions on the basis of 8 O; oxides given in weight percentage -
Table C.8+9: Microprobe analysis of plagioclase and K-feldspar from sample no...
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 2) Major-element compositions of selected primary minerals: plagioclas...
Empty cells indicates concentration below detection limit. All iron in feldspar calculated as Fe3+, as Fe2+ in kaersutite and biotite; Fe3+ in oxides calculated assuming cation... -
(Table 1) Chemical composition of minerals from IODP Hole 305-U1309D
Samples taken between 746.2 and 751.0 mbsf.
