234Th/238U activity ratios in Pacific Ocean bottom waters
Author:
Publisher
Elsevier BV
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Reference11 articles.
1. Trace-element calibrations and profiles at Geosecs test station in the northeast Pacific;Spencer;J. Geophys. Res.,1970
2. 234Th/238U ratios in the Ocean;Bhat;Earth Planet. Sci. Lett.,1969
3. Measurement of228Ra and228Th in seawater;Moore;J. Geophys. Res.,1969
4. The residence time of thorium in surface seawater and its implications regarding the rate of reactive pollutants;Broecker;Earth Planet. Sci. Lett.,1973
5. Sediment transport and distribution in the Argentine Basin, 3. Nepheloid layer and processes of sedimentation;Ewing,1971
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1. 230Th and 232Th distributions in mid-latitudes of the North Pacific Ocean: Effect of bottom scavenging;Earth and Planetary Science Letters;2012-07
2. A review of present techniques and methodological advances in analyzing 234Th in aquatic systems;Marine Chemistry;2006-08
3. An introduction to the application and future use of 234Th in aquatic systems;Marine Chemistry;2006-08
4. Chapter 5 Reactive radionuclides as tracers of oceanic particle flux;Marine Radioactivity;2005
5. Short-lived U/Th Series Radionuclides in the Ocean: Tracers for Scavenging Rates, Export Fluxes and Particle Dynamics;Reviews in Mineralogy and Geochemistry;2003-01-01
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