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(Table 6) Geochemistry of calcium carbonates and associated minerals at DSDP ...
Empty cells mean no data. -
(Table 8) Geochemistry of zeolites at DSDP Hole 70-504B
Structural formulas are calculated on the basis of 7 oxygens for analcime and 80 oxygens for other zeolites. Empty cells mean no data. -
(Table 9) Geochemistry of bulk rock at DSDP Hole 70-504B
This dataset has no description
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(Table 10) Geochemistry of bulk rock recalculated on a volatile-free basis at...
This dataset has no description
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(Table 3) Major element contents and minerals at DSDP Legs 69-70 Holes
Normative magnetite (mt), which was always a value of 2.18 because Fe2O3 was fixed at a value of 1.5% for the normal calculations, was omitted from the table. -
(Table 4) Major element composition of DSDP 68-501-10-1,69-83 when recalculat...
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 6) Major element composition of DSDP 70-504B-40-2,72-88 when recalcula...
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 5) Major element composition of DSDP 70-504B-36-1,91-110 when recalcul...
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
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 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... -
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 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 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 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 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 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... -
(Table 4) Mineralogical composition of heavy minerals in silt and sand fracti...
This dataset has no description
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(Table 2) Annual mass fluxes, 230Th composition and organic geochemistry of s...
The scavenging of 231Pa and 230Th was investigated in the Atlantic Sector of the Southern Ocean by combining results from sediment trap and in situ filtration studies. We... -
Major and trace elements, Sr-Nd-Pb isotope data of lavas from D. João de Cast...
The D. João de Castro seamount is located on the ultraslow diverging Terceira Rift, Azores. D. João de Castro is a young central volcano (<0.5 Ma) with recent volcanic and... -
Geochemical composition of volcanic glass shards from the sediment core POS51...
To investigate the sedimentary record of the Mid Adriatic Deep (Adriatic sea) and its response to climate/oceanographic changes building a satisfactory depth-age model is...
