Advances in Oceanography by X. Le Pichon, M. Melguen, J. C. Sibuet (auth.), Henry

By X. Le Pichon, M. Melguen, J. C. Sibuet (auth.), Henry Charnock, Sir George Deacon (eds.)

The papers on the basic Symposia of the Joint Oceanographic meeting have been provided by way of authors who were invited to house issues of wide interdisciplinary curiosity. jointly they gave a invaluable account of the current country of marine learn, its proQlems and power. There turns out benefit in publishing them in a single quantity and we're thankful to the authors who kindly agreed to organize their papers for booklet. This has taken a while (and now not all authors chanced on it attainable) yet we are hoping the ensuing quantity remains to be indicative of developments in glossy oceanography. really visible is the best way the utilized points are commencing to play a extra very important half inspite of concerns in regards to the results of the legislations of the ocean on our freedom to make observations. we're specifically thankful to the 4 authors who agreed to provide lectures summarising the paintings of their personal box which was once said on the meeting. We additionally desire to thank the opposite authors, in addition to all serious about the meeting and with the construction of this volume.

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A. D. W. , Societe of Econ. Paleontol. and mineralogists. Spec. public. nO 20 p. 126-186. , 1965, Mineralogy and sedimentation of recent deepsea clay in the Atlantic Ocean and adjacent seas and oceans. Bull. Geol. Soc. , 76 - p. 803-832. F. DASCH, 1968: Source of Argentine Basin Sediment, Southwestern South Atlantic Ocean. Geol. Soc. , Abstracts, p. 28. , V. K. TUREKIAN, 1976: Distribution of calcium carbonate in surface sediments of the Atlantic ocean. Geophys. , vol. 81 nO 15, p. 2595-2603. F.

For such elements as barium and mercury, fossil fuel mobilization to the atmosphere appears to be within an order of magnitude of the river fluxes of these metals to the oceans. Selective volatilization can introduce the more readily volatile materials into the atmosphere in higher concentrations than those that are indicated in Table 4. ) suggest that those elements that will be mobilized more effectively through volatilization processes may be found in the emissions from the dc arc as observed by spectrographers.

MATTHEWS, 1963 : Magnetic anomalies over oceanic ridges. Nature, 199, p. 947-949. P. KENNETT, 1971 : Antarctic bottom water - a major change in velocity during the late Cenozoic between Australia and Antarctica, Science, v. 173, p. 813-813. W. ), studies in Paleo-oceanography, Societe of Econom. Pa1eonto1og. , Spec. , p. 94-120. , 1936 : Das Bodenwasser und die gliederung der At1antischen Tiefsee. Dtsch. At1ant. Expea. "Meteor", 1925-1927, 6, p. 1-106. CLIMATE AND THE COMPOSITION OF SURFACE OCEAN WATERS EDWARD D.

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