-
Oxygen, carbon isotope, trace element and foraminifera assemblages from sedim...
Bottom water samples were analysed in Bergen (Norway) using ICP-OES (Inductively Coupled Plasma - Optical Emission Spectrometry) Agilent Technologies, 720 to measure oxygen in... -
Diatom counts from the sediment core PS97/72-1
This dataset has no description
-
Benthic foraminifera abundance in sediment cores CE18011_VC1 and RH17002_VC7
A remotely operated vehicle mounted (ROV) vibrocorer rig acquired the two cores from the Porcupine Bank Canyon (NE Atlantic) and western Porcupine Bank (NE Atlantic) during the... -
Bulk sediment X-ray diffraction analysis and quantification of mineral phases...
This dataset has no description
-
Bulk sediment X-ray diffraction analysis and quantification of mineral phases...
This dataset has no description
-
Bulk sediment X-ray diffraction analysis and quantification of mineral phases...
This dataset has no description
-
Bulk sediment X-ray diffraction analysis and quantification of mineral phases...
This dataset has no description
-
Bulk sediment X-ray diffraction analysis and quantification of mineral phases...
This dataset has no description
-
Bulk sediment X-ray diffraction analysis and quantification of mineral phases...
This dataset has no description
-
Bulk mineral assemblage with X-ray diffraction of sediment core MD99-2323
This dataset has no description
-
Bulk mineral assemblage via Quantitative Phase Analysis with X-ray diffractio...
This dataset has no description
-
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. Element composition of the Yangla granodiorite
This dataset has no description
