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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 -
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. -
Mineralogical composition of sediment core Sardarya from southeast Iran
The proxy data reported here are measured from a sediment core collected from Lake Sardarya (28° 38' 03" N, 61° 00' 44" E, 2675 m a.s.l.) situated on the western slope of Taftan... -
X-ray diffraction mineralogy of sediment core MD99-2323
Weight % of non-clay and clay minerals based on quantitative X-ray diffraction using the “whole-pattern” Rockjock v6.0 Excel macro program (calibrated with 10% zincite) (Eberl,... -
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,... -
(Table A5) Composition of plagiocalse crystals (n=36) from lava samples recov...
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Results of bulk sediment X-ray diffraction analysis and quantification of min...
This dataset has no description
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Crystallization conditions and compositions of residual melts from the Mid At...
This dataset has no description