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Selected rare-earth composition of manganese nodules from Challenger station 276
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other... -
Geochemical anaylsis from the Talheim loess-paleosol sequence in the Heilbron...
This dataset has no description
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Geochemical anaylsis from the Frankenbach loess-paleosol sequence in the Heil...
This dataset has no description
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(Table 4) Epidote / allanite grains major elements from Penninic metasediment...
The major element chemistry of selected epidote / allanite grains calculated from regions of interest (user-defined polygons) on the SEM-EDS maps. -
(Table S5) Representative analyses of the epidote group minerals of sample VT...
Structural formulae have been calculated on the basis of 12.5 oxygens and 8 cations. All Fe assumed as Fe3+; Fe2+ calculated by charge balance to 25 negative charges. #0 = below... -
(Table S3) Representative analyses of titanite of Valtournenche samples
Structural formulae have been calculated on the basis of 5 oxygens, #0 = below detection limit. -
Oxide concentrations of zircons in sediment core AM04 sample AMQ4
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Oxide concentrations of zircons in ODP Hole 188-1167A sample 1167 A-39
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Oxide concentrations of zircons in ODP Hole 188-1167A sample 1167 A-22
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Oxide concentrations of zircons in ODP Hole 188-1167A sample 1167 A-19
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Oxide concentrations of zircons in ODP Hole 188-1167A sample 1167 A-37
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Oxide concentrations of zircons in ODP Hole 188-1166A upper level sample
This dataset has no description
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Oxide concentrations of zircons in ODP Hole 188-1166A upper level sample
This dataset has no description
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Oxide concentrations of zircons in ODP Hole 119-741A sample JJV741A
This dataset has no description
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Age determination on monazite from Forefinger Point granulites, East Antarcti...
Electron microprobe (EMP) dating on monazite in granulite- facies rocks from Forefinger Point, East Antarctica, yielded dominant ages of 500 Ma on matrix monazites.They are...