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Your search keyword '"Janecek, T. R."' showing total 9 results
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9 results on '"Janecek, T. R."'

3. Collision-related break-up of a carbonate platform (Eratosthenes Seamount) and mud volcanism on the Mediterranean Ridge: preliminary synthesis and implications of tectonic results of ODP Leg 160 in the Eastern Mediterranean Sea

Author

Robertson, A. H. F., primary, Emeis, K.-C., additional, Richter, C., additional, Blanc-Valleron, M.-M., additional, Bouloubassi, I., additional, Brumsack, H-J., additional, Cramp, A., additional, Di Stefano, G. J., additional, Flecker, R., additional, Frankel, E., additional, Howell, M. W., additional, Janecek, T. R., additional, Jurado, M.-J., additional, Kemp, A. E. S., additional, Koizumi, I., additional, Kopf, A., additional, Major, C. O., additional, Mart, Y., additional, Pribnow, D. F. C., additional, Rabaute, A., additional, Roberts, A. P., additional, Rullkötter, J., additional, Sakamoto, T., additional, Spezzaferri, S., additional, Staerker, T. S., additional, Stoner, J. S., additional, Whiting, B. M., additional, and Woodside, J. M., additional

Published
1998
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6. Palaeogene ocean opening south of Tasmania, and palaeoceanographic implications: Preliminary results of clay mineral analyses (ODP Leg 189) | L'ouverture océanique au sud de la Tasmanie durant le Paléogène et ses conséquences paléocéanographiques: Résultats préliminaires de la minéralogie des argiles (Leg ODP 189)

Author

Robert, C. M., Neville Exon, Kennett, J. P., Malone, M. J., Brinkhuis, H., Chaproniere, G. C. H., Ennyu, A., Fothergill, P., Fuller, M. D., Grauert, M., Hill, P. J., Janecek, T. R., Kelly, D. C., Latimer, J. C., Roessig, K. M., Nees, S., Ninnemann, U. S., Nürnberg, D., Pekar, S. F., Pellaton, C. C., Pfühl, H. A., Röhl, U., Schellenberg, S. A., Shevenell, A. E., Stickley, C. E., Suzuki, N., Touchard, Y., Wei, W., and White, T. S.

9. Geologic approach to the long-term history of atmospheric circulation.

Author

Rea DK, Leinen M, and Janecek TR

Abstract

Eolian dust preserved in deep-sea pelagic sediments can be used as a proxy indicator of paleoclimate. Analyses of the particle size, composition, and mass accumulation rate of dust grains provide independent evidence of the intensity of atmospheric circulation and the availability of material in the eolian source region. These data provide information on atmospheric circulation and on the climate of the source area at time scales ranging from 103 to 108 years and have the potential to test computer-generated global circulation models.

Published
1985
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