Source and climatic implication of the reactive iron and reactive silicate concentration found in a core from Meserve Glacier, Antartica
Open Access
- 1 March 1982
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 9 (3) , 190-192
- https://doi.org/10.1029/gl009i003p00190
Abstract
No abstract availableThis publication has 13 references indexed in Scilit:
- Microparticle Concentration Variations Linked with Climatic Change: Evidence from Polar Ice CoresScience, 1981
- Sodium, magnesium, potassium and calcium concentrations in ice cores from the Law Dome, AntarcticaGeochimica et Cosmochimica Acta, 1981
- Polar ice evidence that atmospheric CO2 20,000 yr BP was 50% of presentNature, 1980
- Shallow core snow chemistry of Athabasca Glacier, AlbertaCanadian Journal of Earth Sciences, 1980
- Sources of twelve trace metals in Antarctic snows determined by principal component analysisJournal of Geophysical Research, 1980
- Reduction of contamination problems in sampling of antarctic snows for trace element analysisAnalytica Chimica Acta, 1979
- Trace metals in Antarctic snows since 1914Nature, 1979
- Chemistry of polar snows. Estimation of rates of deposition in AntarcticaGeochimica et Cosmochimica Acta, 1972
- Ferrozine---a new spectrophotometric reagent for ironAnalytical Chemistry, 1970
- Contribution to the Movement and the form of Ice Sheets in the Arctic and AntarcticJournal of Glaciology, 1961