234U 238U and 230Th 234U activity ratios in mineral phases of a lateritic weathered zone
- 31 August 1986
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 50 (8), 1697-1702
- https://doi.org/10.1016/0016-7037(86)90131-6
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Extraction Techniques for Selective Dissolution of Amorphous Iron Oxides from Soils and SedimentsSoil Science Society of America Journal, 1983
- Isotopic Disequilibrium of Uranium: Alpha-Recoil Damage and Preferential Solution EffectsScience, 1980
- Evidence for a higher natural uranium content in world riversNature, 1979
- Pitchblende and galena ages in the Alligator Rivers region, Northern Territory, AustraliaMineralium Deposita, 1976
- Partitioning of Trace Metals in Selective Chemical Fractions of Nearshore SedimentsEnvironmental Letters, 1975
- DISSOLUTION OF TRIOCTAHEDRAL LAYER SILICATES BY AMMONIUM OXALATE, SODIUM DITHIONITE–CITRATE–BICARBONATE, AND POTASSIUM PYROPHOSPHATECanadian Journal of Soil Science, 1972
- Uranium isotopes in sea-floor phosphoritesGeochimica et Cosmochimica Acta, 1970
- An evaluation of the U234/U238method as a tool for dating pelagic sedimentsJournal of Geophysical Research, 1965
- Chemical dissolution techniques in the study of soil clays: Part IIClay Minerals, 1965
- Chemical dissolution techniques in the study of soil clays: Part IClay Minerals, 1965