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(Table 1) Mineralogical composition of sediments from DSDP Sites 69-504 and 6...
We discuss the provenance of minerals detected by X-ray-diffraction analyses of sediments of Sites 504 and 505 of Deep Sea Drilling Project Leg 69. These are X-ray-amorphous... -
(Table 6) Mineralogy of sediment core ARA2B-1B
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... -
Quantitative Mineralogy for 34 sediment samples from various circum-Arctic re...
Quantitative mineralogy was determined using the RockJock program (USGS, 2003). United States Geological Survey (USGS) 2003. User's Guide to RockJock -- A Program for... -
(Table 9) Mineralogy, geochemistry and benthic foraminifera of sediment core...
This dataset has no description
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(Table 1) Clay and non-clay mineral composition of dirty ice samples from acr...
Extensive dirty ice patches with up to 7 kg/m**2 sediment concentrations in layers of up to 10 cm thickness were encountered in 2005 and 2007 in numerous areas across the... -
Microwave-induced self-organization in mineral systems. III. FeCl3 colloid (2...
Microwave-induced self-organization of membraneous structures with different morphology in hydrolized FeCl3 colloid (200 W, 2.45 GHz,1 min). The local MW treatment conditions... -
Microwave-induced self-organization in mineral systems. IV. FeCl3 colloid (45...
Membraneous structure self-organization in FeCl3 colloids under microwave treatmet (450 W, 2.45 GHz) occurs due to the hydrolytic polycondensation of the ferric oxohydroxides. A... -
Microwave-induced self-organization in mineral systems. V. FeCl3 colloid (800...
Microwave-induced self-organization in FeCl3 colloids under high irradiation power (800 W) is strongly dependent on the layer thickness of the precursor (saturated ferric... -
Bulk mineral assemblage via Quantitative Phase Analysis with X-ray diffractio...
This dataset has no description
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Bulk mineral assemblage with X-ray diffraction of sediment core MD99-2323
This dataset has no description
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Mineral accumulations during the retreat of the Smith Sound ice stream in the...
This dataset has no description
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Mineral accumulations during the retreat of the Smith Sound ice stream in the...
This dataset has no description
