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Seawater carbonate chemistry and carbon isotope values (delta 13C) in the mus...
Ocean acidification (OA) and global warming present future challenges for shell producing organisms such as mussels through reduction in the carbonate available to produce... -
(Table 5) U/Pb dating on monazite and zircon from leucogranite results (Rennes)
This dataset has no description
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(Table 2) Chalcopyrite and Sphalerite geochemistry of the Ermioni Volcanogeni...
All percentages in wt%. -
(Table 1) Pukeonake whole rock, glass and glass inclusion compositions
Matrix glasses and glass inclusion major elements were measured by electron microprobe, whole rock major elements were determined by XRF and whole rock trace element analyses... -
(Table 2) Selected analyses for garnet pyroxenite and amphibolite samples fro...
Garnet pyroxenite samples = W216, W218, W240, W242A and garnet amphibolite samples = W232, W251, W334. -
(Table 4) Light element contents of minerals of ODP Holes 207-1272A and 207-1...
Sediment depth is given in mbsf. 1 sigma showed as example of measurement errors. -
(Appendix 5) Trace element composition of serpentine, brucite pseudomorphs, a...
This dataset has no description
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(Appendix 5) Major, minor and trace element composition of vein and replacive...
This dataset has no description
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(Appendix 4) Average trace element concentrations in relict olivine, orthopyr...
This dataset has no description
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(Table 2) Trace element composition of serpentine and seprentine-hydroxide ph...
This dataset has no description
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(Table 2) Selected electron microprobe and LA-ICP-MS analyses of spinel, oliv...
This dataset has no description
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(Table 3) Distribution of planktonic foraminifera in ODP Hole 183-1138A, Part...
cf. = uncertain identification, transitional forms, ? = questionable identification. -
(Table 3) Distribution of planktonic foraminifera in ODP Hole 183-1138A, Part II
cf. = uncertain identification, transitional forms, ? = questionable identification. -
(Table 3) Distribution of planktonic foraminifera in ODP Hole 183-1138A, Part I
cf. = uncertain identification, transitional forms, ? = questionable identification. -
(Table 2) Distribution of planktonic foraminifera in ODP Hole 183-1136A
Abundances: AA = very abundant (>40%), A = abundant (26-39%), C = common (16-25%), F = few (6-15%), R = rare (2-5%), VR = very rare (<2%), cf. = uncertain identification,... -
(Table 1) Distribution of planktonic foraminifera in ODP Hole 183-1135A, Part II
Abundances: AA = very abundant (>40%), A = abundant (26-39%), C = common (16-25%), F = few (6-15%), R = rare (2-5%), VR = very rare (<2%), cf. = uncertain identification,... -
Microprobe analyses of orthopyroxene from eclogite and pyroxenite xenoliths, ...
For classification of the minerals and to clarify the geological evolution of the samples major ele-ments of clinopyroxene, orthopyroxene, and olivine (given as oxides in wt.%)... -
Microprobe analyses of olivine from eclogite and pyroxenite xenoliths, Kaapva...
For classification of the minerals and to clarify the geological evolution of the samples major ele-ments of clinopyroxene, orthopyroxene, and olivine (given as oxides in wt.%)... -
Microprobe analyses of clinopyroxene from eclogite and pyroxenite xenoliths, ...
For classification of the minerals and to clarify the geological evolution of the samples major ele-ments of clinopyroxene, orthopyroxene, and olivine (given as oxides in wt.%)...
