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  • Other Sources  (15)
  • Elsevier  (8)
  • Cambridge University Press  (4)
  • Oxford Univ. Press  (2)
  • AGU (American Geophysical Union)  (1)
  • 1960-1964  (15)
  • 1
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    The Friction and Lubrication of Solids: Parts I and II (1964)
    Oxford Univ. Press
    In:  Oxford, Oxford Univ. Press, vol. 3, pp. 158, (ISBN 0-444-50968-2)
    Details
    Publication Date: 1964
    Keywords: Textbook of physics ; Friction ; Physical properties of rocks ; Fluids
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Theory of Probability (1961)
    Oxford Univ. Press
    In:  Oxford, 3rd Edition, 459 pp., Oxford Univ. Press, vol. 46, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Details
    Publication Date: 1961
    Keywords: Textbook of mathematics ; Statistical investigations ; Error analysis ; Earthquake hazard
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Strength variation and deformational behavior in anisotropic rock (1964)
    Elsevier
    In:  Professional Paper, State of Stress in the Earth Crust, Amsterdam, Elsevier, vol. 146, no. 16, pp. 281-300, (ISBN 1-4020-1729-4)
    Details
    Publication Date: 1964
    Keywords: CRUST ; Tectonics ; Stress ; Strength ; Anisotropy ; ERYBACKI
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Rostra of cephalopods in oceanic bottom sediments (1964)
    Elsevier
    In:  Deep Sea Research and Oceanographic Abstracts, 11 (1). pp. 113-126.
    Details
    Publication Date: 2017-05-12
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 5
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    Natural convection in a horizontal circular cylinder (1964)
    Cambridge University Press
    In:  Journal of Fluid Mechanics, 18 (03). pp. 409-437.
    Details
    Publication Date: 2020-07-24
    Description: In this paper we examine the steady, two-dimensional convective motion which occurs in a horizontal circular cylinder whose wall is non-uniformly heated. One observes several qualitatively different physical phenomena depending on the wall temperature distribution and the value of the Rayleigh number. The low-Rayleigh-number behaviour for the single convective cell heated from below is related to the classical Rayleigh stability problem. The critical Rayleigh number for the single circular cell is approximately five times the value for Rayleigh's multi-celluar configuration. The flow which exhibits a nearly parabolic velocity profile near the critical Rayleigh number, gradually changes to a rigidly-rotating-core behaviour as the Rayleigh number increases. The speed of core rotation is a function of the Prandtl number, whereas the boundary-layer thickness is primarily a function of the Rayleigh number. When the heating is from side to side, the solution shows that as the Rayleigh number increases the core motion is progressively arrested leaving a narrow circulating band of fluid adjacent to the wall. An oblique heating produces a hybrid phenomenon, a low-Rayleigh-number behaviour which is characteristic of the sideways heating case and a high-Rayleigh-number interior motion characteristic of the bottom heating case. To determine the core motion in the high-Rayleigh-number limit, Batchelor's work concerning the uniqueness of incompressible, exactly steady, closed streamline flows with small viscosity is extended to include flows with small thermal conductivity.
    Type: Article , PeerReviewed
    Format: text
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  • 6
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    The Gneisses of the Bartica Assemblage, British Guiana (1962)
    Cambridge University Press
    In:  Geological Magazine, 99 (02). pp. 164-172.
    Details
    Publication Date: 2020-07-31
    Description: The results of an examination of one quarry within the gneisses of the Bartica Assemblage are described and the validity of these results throughout the whole of the Bartica Assemblage is discussed. The foliation and banding of the gneisses at Kereti Quarry are mainly the results of tectonism; concomitant metamorphism within the Amphibolite Facies was succeeded by a two-phase metasomatism involving successive additions of Na and K. These results appear valid throughout the Bartica Assemblage and it is further suggested that the main rock type distribution in the Bartica Assemblage is also controlled by tectonism.
    Type: Article , PeerReviewed
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  • 7
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    Porphyroblastic and augen gneisses in the Bartica Assemblage, British Guiana (1964)
    Cambridge University Press
    In:  Geological Magazine, 101 (6). pp. 541-547.
    Details
    Publication Date: 2020-07-31
    Description: Textural differences in the occurrence of microcline define augen gneisses, subhedral porphyroblastic gneisses and euhedral porphyroblastic gneisses within the Bartica Assemblage, British Guiana. The introduction of microcline is metasomatic and the nature of the porphyroblasts appears to be a reflection of tectonic control during their development.
    Type: Article , PeerReviewed
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  • 8
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    A statistical analysis of the generation of microseisms (1963)
    AGU (American Geophysical Union)
    In:  Reviews of Geophysics, 1 (2). pp. 177-210.
    Details
    Publication Date: 2016-09-12
    Description: Theories of the origin of microseisms have in the past generally been expressed in terms of the Green functions of the elastic systems considered. An alternative approach based on spectral transfer functions and the local energy-balance equation of the seismic field is proposed. The method enables a rigorous analysis of the statistical aspects of the problem, which could be treated only approximately and under restrictive conditions in terms of the far-field representations used previously. Three suggested origins of microseisms are considered: (1) the action of ocean waves on coasts, originally proposed by Wiechert; (2) atmospheric pressure fluctuations, as suggested by Gherzi, Scholte, and others; and (3) nonlinear interactions between ocean waves as proposed by Longuet-Higgins. In all cases appreciable microseisms are generated only by Fourier components of the random exciting fields that have the same phase velocities as free modes of the elastic system. The effect of pressure fluctuations associated with turbulence in the atmosphere is found to be negligible. The theory for Wiechert's and Longuet-Higgins' mechanisms is in good agreement with recent measurements by Haubrich et al.
    Type: Article , PeerReviewed
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  • 9
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    On the in situ measurement of temperature and electrical conductivity of sea-water (1963)
    Elsevier
    In:  Deep Sea Research and Oceanographic Abstracts, 10 (3). pp. 269-277.
    Details
    Publication Date: 2016-09-22
    Description: After some brief comments on the measurement of temperature and electrical conductivity in oceanography, the measuring probes suitable for in situ measurements are reviewed. Then the method of measurement is described using an improved model of the so-called bathysonde. This makes possible a continuous recording of temperature, conductivity, and pressure with high accuracy in great depths. Measurements from the Skagerrak and from the Mediterranean are considered. Finally, problems are discussed which arise when evaluating electrical conductivity and temperature from in situ measurements.
    Type: Article , PeerReviewed
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  • 10
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    On the processes of renewal of the North Atlantic deep water in the Irminger Sea (1964)
    Elsevier
    In:  Deep Sea Research and Oceanographic Abstracts, 11 (6). pp. 881-890.
    Details
    Publication Date: 2016-09-22
    Description: Observations of temperature and electrical conductivity by a recording in situ salinometer are discussed in respect oo the physical processes connected with the renewal of North Atlantic deep water. The measured fine structure of the layering suggests that the downward movement of cooled surface water is combined with horizontal mixing down to more than 1000 m depth. This is confirmed by the existence of water elements which have slightly different temperature and salinity. Curves of temperature, conductivity, and salinity and T-S diagrams are shown.
    Type: Article , PeerReviewed
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