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(Table 3) Accumulation rates of major and trace elements from ODP Hole 175-1085A
This dataset has no description
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XRF-Scan Data from the southeast Pacific sediment core MR16-09 PC03
This dataset has no description
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XRF analysis of sediment core M125-35-3
This dataset has no description
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Major elements (XRF) of sediment core MD97-2142 during MARION DUFRESNE cruise...
Major elements (Si, Ti, Al, Fe, Mn, Mg, Ca, Na, K, P) were measured with conventional XRF (RIGAKU RIX2000 X-ray fluorescence spectrometer at the Department of Geosciences at... -
Geochemistry of sediment core GeoB2910-1
This dataset has no description
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Geochemistry of sediment core GeoB1523-1
This dataset has no description
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Geochemistry of sediment core GeoB1505-2
This dataset has no description
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Geochemistry of sediment core GeoB3176-1
This dataset has no description
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Geochemistry of sediment core GeoB3117-1
This dataset has no description
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Geochemistry of sediment core GeoB1117-2
This dataset has no description
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Geochemistry of sediment core GeoB1112-4
This dataset has no description
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Geochemistry of sediment core GeoB1101-5
This dataset has no description
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Geochemistry of sediment core GeoB4901-8
This dataset has no description
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(Table 7) Accumulation rates for sediments from ODP Hole 115-711A
Major element given as oxides. -
(Appendix) Temporal variations of Fe, Mn, Ti and Cu accumulation rates in met...
This dataset has no description
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(Appendix) Different accumulation rates from ODP Hole 189-1172A
This dataset has no description
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(Appendix) Different accumulation rates from ODP Hole 189-1171A
This dataset has no description
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(Appendix) Different accumulation rates from ODP Hole 189-1170A
This dataset has no description
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(Appendix) Different accumulation rates from ODP Hole 189-1168A
This dataset has no description
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A pair distribution function study to determine the local structure of the ti...
BaTiO3 is the prototypical ferroelectic perovskite and has been well studied for over 60 years. The standard structural picture is that it is cubic and paraelectric at high...
