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X-ray diffraction mineralogy of sediment core MD99-2323
Weight % of non-clay and clay minerals based on quantitative X-ray diffraction using the “whole-pattern” Rockjock v6.0 Excel macro program (calibrated with 10% zincite) (Eberl,... -
X-ray diffraction results from IODP Hole 381-M0080A
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
X-ray diffraction results from IODP Hole 381-M0079A
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
X-ray diffraction results from IODP Hole 381-M0078B
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
X-ray diffraction results from IODP Hole 381-M0078A
Data were measured with: Philips X'Pert Pro multipurpose diffractometer with a Philips back-loading system and Philips software X'Pert HighScore™. -
Bulk sediment mineral composition of sediment core GeoB12605-3
Equatorial East Africa experienced significant variations in paleoclimatic and paleoceanographic conditions during the Holocene. These environmental changes influenced... -
(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... -
Detrital minerals and coarse component composition of sediment core LV83-16-1...
This data includes sediment detrital mineral data and coarse component composition data. Detrital minerals are obtained from sediment in the 0.063-0.25 mm grain size fraction... -
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,... -
Mineralogy and cation exchange capacity obtained from Röttingen core
XRD patterns of whole rock material were recorded using a PANalytical X'Pert PRO MPD θ - θ diffractometer (Co-Kα radiation generated at 40 kV and 40 mA). The samples were... -
Mineralogy and cation exchange capacity obtained from Metzingen core
XRD patterns of whole rock material were recorded using a PANalytical X'Pert PRO MPD θ - θ diffractometer (Co-Kα radiation generated at 40 kV and 40 mA). The samples were... -
Bulk mineral assemblage via Quantitative Phase Analysis with X-ray diffractio...
This Hi-resolution quantitative phase analysis XRD data set was prepared initially at the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI) in 1997.... -
(Table 1) Mineral composition and d-spacing of montmorillonite and montmorill...
Sediment depth is given in mbsf. d-spacing (Å) of Montmorillonite-illite mixed-layer represented by 10 Å peak with tailed reflections on the lower angle side. -
(Table 1) Mineralogy at DSDP Hole 62-463
?1 = presence uncertain epmty cells = no data. -
(Table 3) Mineralogy at DSDP Hole 80-550
Sediment depth is given in mbsf. Bulk sediment contained no dolomite, aragonite, or anhydrite. -
(Table 2) Mineralogy at DSDP Site 80-549
Sediment depth is given in mbsf. Bulk sediment contained no dolomite, aragonite, or anhydrite. -
(Table 1) Mineralogy at DSDP Site 80-548
This dataset has no description
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(Table 3) Relative abundance of carbonate minerals in ODP Leg 164 sites
This dataset has no description
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(Table 3) XRD intensities of carbonate minerals from ODP Hole 164-997A under ...
All intensities were originally given in counts/min which had been calibrated by standard quartz count. -
(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.
