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Detailed Reference Information |
Mayewski, P.A. and Lyons, W. B. (1982). Source and climatic implication of the reactive iron and reactive silicate concentration found in a core from Meserve Glacier, Antartica. Geophysical Research Letters 9. doi: 10.1029/GL009i003p00190. issn: 0094-8276. |
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Data is presented suggesting that there may be a local source in some cases for the crustally-derived material that enters Antartic precipitation.(AIP) |
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Abstract |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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