Oxygen isotopes in an oolitic ironstone and the determination of goethite δ18O values by selective dissolution of impurities: The 5M NaOH method
- 1 September 1991
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 55 (9) , 2627-2634
- https://doi.org/10.1016/0016-7037(91)90378-i
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- The implication of the oxygen isotope records in coexisting cherts and phosphatesGeochimica et Cosmochimica Acta, 1986
- Isolation of diagenetic overgrowths on quartz sand grains for oxygen isotopic analysisGeochimica et Cosmochimica Acta, 1985
- Stable hydrogen isotopes in iron oxides—isotope effects associated with the dehydration of a natural goethiteGeochimica et Cosmochimica Acta, 1983
- The 5-M-NaOH Concentration Treatment for Iron Oxides in SoilsClays and Clay Minerals, 1982
- Paleozoic Base MapsThe Journal of Geology, 1979
- Standards for stable isotope measurements in natural compoundsNature, 1978
- Particle size effect on the reaction goethite = hematite + waterAmerican Journal of Science, 1971
- Stable isotopes in precipitationTellus, 1964
- A method of analysis of oxygen isotopes in orthophosphate—its use in the measurement of paleotemperaturesGeochimica et Cosmochimica Acta, 1960
- Variation of O18 content of waters from natural sourcesGeochimica et Cosmochimica Acta, 1953