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XRD mineralogical abundances in sediments off Milos, Greece
Mineralogical abundances from XRD reported as weight percent (values normalized to 1 = 100%). -
(Table 1) Quantitative mineralogy at DSDP Holes 59-447A and 59-450
The authigenic minerals contained in the altered basal intervals of volcaniclastic sediments from Sites 447 and 450 of Deep Sea Drilling Project Leg 59 are dioctahedral smectite... -
Smear slide investigation on ODP Hole 202-1239A
This dataset has no description
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Smear slide investigation on ODP Hole 202-1237B
This dataset has no description
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Smear slide investigation on ODP Hole 202-1237A
This dataset has no description
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(Table 3) Occurrence of secondary minerals in in veins and vesicles of basalt...
Sediment depth is given in mbsf. P = present; ? = uncertanty. -
(Table 28) Minerals from veins in basalts of the Costa Rica Rift
X - mixed-layer chlorite-montmorillonite mineral; X* - analysis of thomsonite has been obtained from N.N. Pertsev. -
(Fig. 7) Distribution of secondary minerals in basalts of the Costa Rica Rift...
This dataset has no description
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(Appendix A) Hematite, goethite concentrations, reflectance in color bands an...
This dataset has no description
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(Table 1) Hematite, goethite concentrations, reflectance in color bands and t...
Sediment depth (m) is composite depth (mcd) -
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... -
Dry powders reflectance model based on enhanced backscattering: case of hemat...
Data associated to the paper entitled: Morgane Gerardin, Pauline Martinetto, and Nicolas Holzschuch, "Dry powders reflectance model based on enhanced backscattering: case of... -
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...
