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  • Other Sources  (10)
  • Springer  (6)
  • Elsevier  (4)
  • Annual Reviews
  • Frontiers Media
  • 2020-2022
  • 1980-1984
  • 1970-1974  (10)
  • 1974  (10)
  • 1
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    Spectral Analysis in Geophysics (1974)
    Elsevier
    In:  Amsterdam, Elsevier, vol. 8, pp. 415, (ISBN 0-471-95596-5)
    Details
    Publication Date: 1974
    Keywords: Textbook of geophysics ; Data analysis / ~ processing ; Spectral analysis ; Spectrum ; Seismology ; Seismics (controlled source seismology) ; Bath
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Global Tectonics and Earthquake Risk (1974)
    Elsevier
    In:  Amsterdam, London, New York, xiv+320 pp., Elsevier, vol. 5, no. 22, pp. 662-664, (ISBN 1-4020-1244-6)
    Details
    Publication Date: 1974
    Keywords: Earthquake risk ; Earthquake hazard ; Earthquake engineering, engineering seismology ; Seismicity ; Plate tectonics ; Tectonics ; Seismology
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    The fine-structure contamination of vertical velocity spectra in the deep ocean (1974)
    Elsevier
    In:  Deep Sea Research and Oceanographic Abstracts, 21 (1). pp. 37-46.
    Details
    Publication Date: 2018-03-08
    Description: When determining vertical velocity spectra from temperature time series and the mean vertical temperature gradient, restrictions may arise friom the existence of fine-structre. Phillips (1971) and Garrett and Munk (1971_ have shown that the fine-structure contamination of internal gravity wave spectra can be written as a function of some statistical properties of the internal wave field and the vertical wave number spectrum of the fine-structure. A consistent set of current and temperature data was obtained during an experiment at Site D to study this problem. The wave number spectrum of the vertical temperature fine-structure and the apparent frequently spectrum of internal waves are determined from these data. In contrast to the asasumptions in the above models, our fine-structure data imply a wave number spectrum proportional to (wave number)−3 in the range which is important here. Using the above set of data, a model is suggested to describe the effect of fine-structure on vertical velocity spectra computed with the mean vertical temperature gradient. It indicates a maximum fine-structure contamination of the true frequency spectrum of internal gravity waves in the middle of the internal wave band, with less contamination at low and high frequencies.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 4
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    Temperatur, Salzgehalt und Dichte (1974)
    Springer
    In:  In: Meereskunde der Ostsee. , ed. by Magaard, L. and Rheinheimer, G. Springer, Berlin, Germany, pp. 46-60.
    Details
    Publication Date: 2013-05-14
    Type: Book chapter , NonPeerReviewed
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  • 5
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    Wasserhaushalt und Strömungen (1974)
    Springer
    In:  In: Meereskunde der Ostsee. , ed. by Magaard, L. and Rheinheimer, G. Springer, Berlin, pp. 33-41.
    Details
    Publication Date: 2019-09-23
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 6
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    Observations of internal wave coherence in the deep ocean (1974)
    Elsevier
    In:  Deep Sea Research and Oceanographic Abstracts, 21 (8). pp. 597-610.
    Details
    Publication Date: 2016-09-22
    Description: An experiment is described which was aimed at testing assumptions and predictions of the internal wave model suggested by Garrett and Munk (1972). Two moorings were set at a depth of 2660 m with a horizontal separation of 920 m only. The results of current and temperature measurements on these moorings indicate that the field of motion is probably horizontally isotropic in the inertio-gravitational wave band. The limiting frequency for horizontal coherence is three times the frequency predicted by the theoretical model. The phase of the vertical coherence is stable over a wide frequency range and the coherence decreases towards higher frequencies. This may be due to coherent motion contaminated by uncorrelated noise at high frequencies. The results are basically in agreement with the theoretical model when taking a number of modes below 10.
    Type: Article , PeerReviewed
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  • 7
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    Laboratory observations on spawning and embryonic development of a blue-ringed octopus (1974)
    Springer
    In:  Marine Biology, 27 (4). pp. 333-337.
    Details
    Publication Date: 2016-09-15
    Description: A female blue-ringed octopus, Hapalochlaena sp. (probably lunulata), was maintained in an aqarium for nearly 3 months, during which time it spawned and cared for the eggs until hatching. The young are planktonic. Embryonic development does not differ markedly from that observed in other octopods, uniting certain features of the development of Octopus vulgaris and Eledone cirrosa. In terms of reproductive biology and development, the species differs from the lesser blue-ringed octopus Hapalochlaena maculosa in its mode of spawning, egg size and mode of life of its young. These differences correspond to conditions recorded for Octopus spp. and Eledone spp.
    Type: Article , PeerReviewed
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  • 8
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    Eisverhältnisse (1974)
    Springer
    In:  In: Meereskunde der Ostsee. , ed. by Magaard, L. and Rheinheimer, G. Springer, Berlin, Germany, pp. 61-66. ISBN 3-540-06897-X
    Details
    Publication Date: 2016-07-13
    Type: Book chapter , NonPeerReviewed
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  • 9
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    Untermeerische mineralische Rohstoffe in den Ozeanen (1974)
    Springer
    Details
    Publication Date: 2022-03-10
    Description: Mineral resources on and beneath the seafloor are briefly reviewed and the present and future economic value of specific mineral resources is discussed. The results obtained from the cruises of the German research vessel "Valdivia" during its first three years of operation are presented.
    Type: Article , PeerReviewed
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  • 10
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    Deep-Sea Carbonates (1974)
    Springer
    Details
    Publication Date: 2023-11-24
    Description: Calcium carbonate in sediments can greatly effect the engineering properties of those sediments. Factors that may effect engineering properties are: 1) great variation in primary void ratios, (2) inherent strength of carbonate grains, (3) degree of sorting, (4) ratio between grains and matrix, (5) nature and amount of cement, and (6) depth of burial. Deep-sea carbonates appear to be anomalous but do exist in rather large quantities. Their existence must depend upon a combination of physico-chemical and organic-chemical factors that need to be investigated in much more detail.
    Type: Book chapter , NonPeerReviewed
    Format: text
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