Oxygen isotopic ratios in quartz as an indicator of provenance of dust

Oxygen isotopic ratios in quartz as an indicator of provenance of dust [electronic resource]

Quartz was isolated in the long range aerosol size range (fine silt, 1-10 ..mu..m in diameter) from atmospheric aerosols, wind-erosive soils, soil silts, shales, and Pacific pelagic sediments of the Northern and Southern Hemispheres, to trace their provenance or origin, as part of a study of dust mi...

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Bibliographic Details
Online Access: Online Access
Corporate Authors: Alabama A & M University (Researcher), United States. Department of Energy. Chicago Operations Office (Researcher)
Format: Government Document Electronic eBook
Language:English
Published: Washington, D.C. : Oak Ridge, Tenn. : United States. Energy Research and Development Administration. ; distributed by the Office of Scientific and Technical Information, U.S. Department of Energy, 1977.
Subjects:
Oxygen Isotopes.
Beta Decay Radioisotopes.
Shales.
Silicon Oxides.
Chemical Composition.
Rocks.
Beta-minus Decay Radioisotopes.
Soils.
Even-even Nuclei.
Cesium 137.
Aerosols.
Stable Isotopes.
Isotopes.
Erosion.
Isotope Ratio.
Oxygen Compounds.
Oxygen 18.
Oxygen 16.
Silt.
Dispersions.
Dusts.
Colloids.
Weathering.
Odd-even Nuclei.
Alkali Metal Isotopes.
Cesium Isotopes.
Quartz.
Silicon Compounds.
Origin.
Metamorphic Rocks.
Chemical Analysis.
Oxides.
Sols.
Light Nuclei.
Nuclei.
Years Living Radioisotopes.
Radioisotopes.
Chalcogenides.
Environmental Sciences.
Inorganic, Organic, Physical And Analytical Chemistry.

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Call Number: E 1.99: conf-770210-11
E 1.99: conf-770210-11 Available

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