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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) Apparent ages from 40Ar/39Ar heating steps for DSDP Hole 72-516F ba...
Submarine basalts are difficult to date accurately by the potassium-argon method. Dalrymple and Moore (1968) and Dymond (1970), for example, showed that, when the conventional... -
(Table 1) 40Ar-39Ar incremental heating ages for ODP Hole 163-988A basalt and...
Results of 40Ar-39Ar Ar dating constrain the age of the submerged volcanic succession, part of the seaward-dipping reflector sequence of the Southeast Greenland volcanic rifted... -
(Table 1) 40Ar/39Ar plateau and isochron ages for basalts from the Réunion ho...
Concordant plateau and isochron ages were calculated from 40Ar/39Ar incremental heating experiments on volcanic rocks recovered by drilling at four Leg 115 sites and two... -
39Ar/40Ar ratios of whole rock samples from ODP Hole 107-655B and 107-651A (T...
Six whole rocks from the basaltic lava series drilled in the Vavilov basin have been analyzed by 39Ar-40Ar stepwise heating method. One sample from the upper part of the Hole... -
(Table DR1) Argon isotope data and dating for individual >63 µm amphibole gra...
Variations of global and regional silicate weathering rates and paleo-ocean circulation patterns are estimated by using radiogenic isotope records, but the effects of changes in... -
(Table S3) Argon geochemistry of minerals from Hawaiian-Emperor seamounts
Position of the seamounts are estimated. The parameter J, a measure of the extent of conversion of 39K to 39Ar, was determined for each sample by analyzing co-irradiated Fish... -
(Table 4) 40Ar-39Ar data of white mica single grains from East Antarctica
This dataset has no description
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(Table 3) 40Ar-39Ar data of samples from East Antarctica
This dataset has no description
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(Table 2) In situ 40Ar-39Ar data on rock chip from samples in East Antarctica
This dataset has no description
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(Table 1) 40Ar/39Ar plateau and isochron ages from on-land Caribbean plateau ...
AGE is the plateau age. Postions are a rough estimation from map -
40Ar/39Ar ages from muscovite collected in the far western Nepal Himalaya: Ra...
This dataset contains the cooling age results of 3 individual 40Ar/39Ar analyses using muscovite extracted from bedrock samples collected from medium-high grade metamorphic...
