995 resultados para Ronne Antarctic Research Expedition, 1946-1948


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From the above and the grafical results it can be concluded that cores in the research area are locally dominated by turbiditic sequences, which can be observed by a strong increase in coarser sediment (>35 µm). These coarser intercalations are lacking in the vicinity of basaltic seamounts, probably due to a shadowing effect of the seamounts. The infill of the King George Basin might be dominated by a north eastern current. Sedimentary structures as observed in the cores are often lacking or vague due to hydrothermal effects (Suess, L, 1986).

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"Presented in preliminary form as Appendix H at the Annual Meeting of the Division, May 2, 1947."

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Mode of access: Internet.

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Mode of access: Internet.

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v. 1. Summarization, fundamental and applied research.--v. 2. Fundamental properties, clay - water systems.--v. 3. Applied research, chrome-lignin process and soil briquetting.

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Report prepared by History Associates, Inc. under subcontract no. 19X22268 for Oak Ridge National Laboratory for the U.S. Dept. of Energy.