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(Table 6) Geochemistry of zeolites at DSDP Holes 68-501 and 69-504B
Number of cations is based on 32 oxygens. -
(Table 8) Geochemistry of mineral tentatively identified as anhydrite at DSDP...
This dataset has no description
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(Table 7) Geochemistry of carbonates at DSDP Hole 69-504B
This dataset has no description
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(Table 4) Geochemistry of iddingsites fron DSDP Hole 70-504B
Structural formulas are calculated on the basis of 22 oxygens. Al not recalculated for y sum. -
(Table 6) Geochemistry of calcium carbonates and associated minerals at DSDP ...
Empty cells mean no data. -
(Table 7) MgO content of vein calcites at DSDP Holes 69-504B and 70-504B
This dataset has no description
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(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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Geochemical composition of tephra grains on sediment core PS2644-2, raw data
This dataset has no description
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Geochemical composition of tephra grains on sediment core PS2644-5, raw data
This dataset has no description
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Effects of the hydrous domain in the mantle wedge on magma formation and mixi...
Major and trace element concentrations of young volcanic rocks from the Northeast Lau Basin in the SW Pacific Ocean, as well as Sr-Nd-Hf-Pb isotope compositions. Analyses were... -
(Table 2) Major element analyses of glass particles from sediment cores HM79-...
This dataset has no description
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(Table T2) Electron microprobe analyses of iron concentrations within weakly ...
Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (<12 µm) and disseminated nature. -
(Table T2) Electron microprobe analyses of iron concentrations within blocky ...
Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (<12 µm) and disseminated nature. -
(Table T2) Electron microprobe analyses of iron concentrations within blocky ...
Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (<12 µm) and disseminated nature. -
(Table T2) Electron microprobe analyses of iron concentrations within lumines...
Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (<12 µm) and disseminated nature. -
(Table T2) Electron microprobe analyses of iron concentrations within lumines...
Electron microprobe analysis of zoned dolomite was not possible because of its small crystal size (<12 µm) and disseminated nature. -
Major oxides for tektites and for conglomerate clast of the Upper Eocene ejec...
Evidence for the Chesapeake Bay Crater as the source for New Jersey continental margin ejecta is provided by fine-grained tektites and coarse-grained unmelted ejecta. The Upper... -
(Table 1) Composition of matrix glasses of fallout tephra from ODP Hole 125-782A
This dataset has no description