K-Ar dates were obtained for three pillow basalt samples recovered from Site 608 (Samples 608-58-1, 103-109 cm; 608-59-1, 3-7 cm; 608-59-1, 48-53 cm). Reliable K-Ar dates cannot be routinely obtained for deep-sea igneous rocks, because they may be subject to inaccuracies related to seawater alteration (Seidemann, 1977, doi:10.1130/0016-7606(1977)882.0.CO;2) and/or the presence of excess radiogenic 40Ar (Dalrymple and Moore, 1968, doi:10.1126/science.161.3846.1132; Dymond, 1970, doi:10.1130/0016-7606(1970)81[1229:EAISBP]2.0.CO;2). Thus, the possibility that the samples dated in this study were subject to these sources of inaccuracy must be evaluated
Igneous rocks were recovered from three sites on Hess Rise during Deep Sea Drilling Project Leg 62: ...
The CRP-3 core, drilled in western McMurdo Sound in October and November 1999, penetrated 823 m of l...
Hydrothermal circulation at oceanic spreading ridges causes sea water to penetrate to depths of 2 to...
Submarine basalts are difficult to date accurately by the potassium-argon method. Dalrymple and Moor...
Conventional K-Ar ages have been determined and inert-gas abundances have been measured on represent...
40Ar/39Ar geochronological studies were performed on basalts taken from the bottom of Hole 462A. An ...
Recent revisions of the geological time scale by Kent and Gradstein (in press) suggest that, on the ...
Age-progressive, linear seamount chains in the northeast Pacific appear to have formed as the Pacifi...
40Ar/39Ar analyses of tephra and clasts of volcanic rock provide age constraints for upper parts of ...
40Ar-39Ar step-heating dating was applied to a basalt from Hole 462 and to basalt and dolerite sampl...
Ash layers from Deep Sea Drilling Project site 178 in the northeast Pacific Ocean have been dated by...
Several samples from the rhyolitic lavas encountered in Hole 841 B in the Tonga Forearc were made av...
A well-constrained Rb/Sr isochron of secondary celadonites and carbonate from DSDP Hole 516F yields ...
Samples from Holes 147, 147A, and 147B have been dated by the radiocarbon method; ages ranged to 27,...
Despite the different scientific objectives of Legs 185 and 191, the sedimentary sections recovered ...
Igneous rocks were recovered from three sites on Hess Rise during Deep Sea Drilling Project Leg 62: ...
The CRP-3 core, drilled in western McMurdo Sound in October and November 1999, penetrated 823 m of l...
Hydrothermal circulation at oceanic spreading ridges causes sea water to penetrate to depths of 2 to...
Submarine basalts are difficult to date accurately by the potassium-argon method. Dalrymple and Moor...
Conventional K-Ar ages have been determined and inert-gas abundances have been measured on represent...
40Ar/39Ar geochronological studies were performed on basalts taken from the bottom of Hole 462A. An ...
Recent revisions of the geological time scale by Kent and Gradstein (in press) suggest that, on the ...
Age-progressive, linear seamount chains in the northeast Pacific appear to have formed as the Pacifi...
40Ar/39Ar analyses of tephra and clasts of volcanic rock provide age constraints for upper parts of ...
40Ar-39Ar step-heating dating was applied to a basalt from Hole 462 and to basalt and dolerite sampl...
Ash layers from Deep Sea Drilling Project site 178 in the northeast Pacific Ocean have been dated by...
Several samples from the rhyolitic lavas encountered in Hole 841 B in the Tonga Forearc were made av...
A well-constrained Rb/Sr isochron of secondary celadonites and carbonate from DSDP Hole 516F yields ...
Samples from Holes 147, 147A, and 147B have been dated by the radiocarbon method; ages ranged to 27,...
Despite the different scientific objectives of Legs 185 and 191, the sedimentary sections recovered ...
Igneous rocks were recovered from three sites on Hess Rise during Deep Sea Drilling Project Leg 62: ...
The CRP-3 core, drilled in western McMurdo Sound in October and November 1999, penetrated 823 m of l...
Hydrothermal circulation at oceanic spreading ridges causes sea water to penetrate to depths of 2 to...