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(Table 4) Chemical composition of bulk samples from ODP Hole 125-782A fallout...
Numerical ages of tephra are based on calcareous nannofossil stratigraphy Xu and Wise (1992, doi:10.2973/odp.proc.sr.125.142.1992) -
(Table 2) Trace element concentrations of selected Cocos Plate samples
This dataset has no description
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(Table 4) Trace element concentrations of glasses from ODP Site 180-1115
This dataset has no description
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(Table 4) Trace element concentrations of glasses from ODP Hole 180-1109C
This dataset has no description
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Chemical composition of hydrothermal fluids at station MSM04/3-275-ROV-8
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-275-ROV-7
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-275-ROV-5
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-271-ROV-11
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-259-ROV-25
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-3
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-17
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-13
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-12
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-253-ROV-9
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-253-ROV-10
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-244-ROV-7
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Elemental and Mo isotope data (porewater) of multicorer samples from the Guay...
The here presented sample set is from three cores from the Guaymas Basin (Gulf of California), covering a broad range of depositional environments. This includes sediments from... -
(Table 1) Geochemistry of Central American Arc volcanites
This dataset has no description
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(Table 4) Trace element concentrations of glasses from ODP Hole 180-1108B
This dataset has no description
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(Table 1) Boron analyses from ODP Sites 186-1150 and 186-1151
Interstitial pore waters from Ocean Drilling Program (ODP) Sites 1150 and 1151, both penetrating ca. 1200 m of sub-seafloor sediment from the upper Japan Trench forearc, were...
