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(Table 1A) Texture, composition and geochemistry at DSDP Site 93-603
Sediment depth is given in mbsf. D = dominant (>25 [50]%); A = abundant; C = common (> 10%); R = rare; T = traces (< 10 [5]%); (T) = ? traces. #0 = traces. -
(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... -
Smear slide analysis of Hole 93-603C
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Smear slide analysis of Hole 93-603
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Mineral composition of bulk sediment from Hole 27-259
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Mineral composition of silt fraction from Hole 27-259
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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... -
Bulk mineral assemblage of sediment core PS72/413-3 determined via full patte...
The XRD data has been gained from pulverized and homogenized samples each centimeter of core PS72/413-3 GKG by AWI personal at AWI core labs supervised by Drs. Jutta Wollenburg... -
(Table T57) Secondary minerals in fine fraction sampled from igneous rocks of...
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(Table T57) Secondary minerals in fine fraction sampled from igneous rocks of...
This dataset has no description
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(Table T57) Secondary minerals in fine fraction sampled from igneous rocks of...
This dataset has no description
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(Table T57) Secondary minerals in fine fraction sampled from igneous rocks of...
This dataset has no description
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(Table T57) Secondary minerals in fine fraction sampled from igneous rocks of...
This dataset has no description