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(Table 5) Incremental heating and age determination of whole-rock samples fro...
This dataset has no description
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(Table 4) Incremental heating and age determination for whole-rock samples fr...
1100°C = heat each of the previously heated basalt fragments to 1100°C, measure individually. Fuse previously heated basalt fragments, measure in three groups of three fragments... -
(Table 3) Incremental heating and age determination for mineral separates fro...
This dataset has no description
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(Table 2) Incremental heating and age determination for mineral separates fro...
This dataset has no description
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(Table 4) Age determination and argon isotope ratios of igneous rocks of ODP ...
This dataset has no description
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(Table 1) Noble gas elemental abundance of pillow lava in DSDP sites
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(Table 3) Noble gas concentrations of oceanic sediments
This dataset has no description
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(Table 2) Noble gas concentrations of old oceanic crust
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(Table T2) 40Ar-39Ar data on milligram-sized fractions, ODP Hole 178-1097A
178-1097A-27R-1,35-58, (6.8 mg) J = 0.0006101 -
(Table T2) 40Ar-39Ar data on milligram-sized fractions, ODP Hole 178-1103A
178-1103A-36R-3,4-8 (10.7 mg) J = 0.0006055 -
(Table T3) 40Ar-39Ar data on multi-grain fractions, ODP Hole 178-1103A
178-1103A-36R-3,4-8 (30 grains) J = 0.0006055; 178-1103A-31R-2,0-4 (30 grains) J = 0.0006015; Note: the final step was lost for a technical reason. -
(Table T3) 40Ar-39Ar data on multi-grain fractions, ODP Hole 178-1097A
178-1097A-27R-1,35-58 (10 grains) J = 0.0006101 -
(Table 1) K-Ar age and inert-gas-isotopes at DSDP Holes 68-501, 69-504B and 6...
Conventional K-Ar ages have been determined and inert-gas abundances have been measured on representative samples of altered rocks from Deep Sea Drilling Project Holes 501,... -
(Table 1) Downhole variation of potassium, apparent K-Ar age, and inert gas a...
Ne, Ar, Kr, Xe, and K2O were measured in representative samples of holocrystalline basalt from DSDP Hole 504B. No hiatus in inert gas abundance is recognized at the base of the... -
(Table 3) Noble gas composition of dissociated gas hydrate specimens from ODP...
Fractionation of the noble gases should occur during formation of a Structure I gas hydrate from water and CH4 such that CH4 hydrate is greatly enriched in Xenon. Noble gas... -
(Table 1) Concentrations and isotopic ratio of Argon in Cretaceous deep-sea b...
The abundance and isotopic composition of rare gas in the mantle provides an important constraint on the origin and evolution of the Earth's atmosphere. One of sources of such... -
(Table 1) Isotopic composition of noble gases from metasediments
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(Table 1) Noble gas elemental abundance of pillow lava from CYAMEX samples
This dataset has no description
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(Table 4) 40Ar-39Ar data of white mica single grains from East Antarctica
This dataset has no description
