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Quantitative X-ray diffraction replicate results of the weight % of non-clay ...
This dataset has no description
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(Table 3) Mineralogy of selected hydrothermal precipitates from Mid Atlantic ...
This dataset has no description
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Smear slide analysis of core GeoB5556-2
C (common) = >10%, F (frequent) = 1-10%, R (rare) = <1% -
Smear slide analysis of core GeoB5555-5
C (common) = >10%, F (frequent) = 1-10%, R (rare) = <1% / reworked nannofossils in several samples (Cretaceous + Miocene) -
Smear slide analysis of core GeoB5547-3
C (common) = >10%, F (frequent) = 1-10%, R (rare) = <1% / reworked nannofossils in several samples (Cretaceous + Miocene) -
Smear slide analysis of core GeoB5546-2
C (common) = >10%, F (frequent) = 1-10%, R (rare) = <1% -
Hematite stained quartz in sediment core GIK13291-1
Empty cells = not counted. -
Results of bulk sediment X-ray diffraction analysis and quantification of min...
This dataset has no description
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Hematite and goethite concentrations, and reflectance in various color bands ...
Aptian–Albian sediments in Core 12X of Hole 1049C (ODP Leg 171B) are characterized by high-frequency cycles that consist of alternating layers of red and green/white clayey... -
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... -
Micro-inclusions identified with Raman spectroscopy in thirteen samples (1360...
Micro-inclusions in thirteen samples (1360-2115 m) from the Last Glacial of the East Greenland Ice Core Project ice core in North-East Greenland were located with microstructure... -
Locations of micro-inclusions identified with Raman spectroscopy in eleven sa...
Micro-inclusions in eleven samples from the upper 1340 m of the East Greenland Ice Core Project ice core in North-East Greenland were analysed with Raman spectroscopy. Ice... -
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,...
