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  • Other Sources  (7)
  • Wiley  (6)
  • AGU (American Geophysical Union)
  • American Meteorological Society
  • MDPI Publishing
  • Oxford Univ. Press
  • 1965-1969  (7)
  • 1
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    The Application of Modern Physics to the Earth and Planetary Interiors (1967)
    Wiley
    In:  New York, Wiley, vol. 6, no. Publ. No. 12, pp. 81-89, (ISBN 0-444-50971-2)
    Details
    Publication Date: 1967
    Keywords: Textbook of geophysics
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    The solution of linear equations by the conjugate gradient method (1967)
    Wiley
    In:  Mathematical Methods for Digital Computers, Volume 1, Sapporo, Japan, Wiley, vol. 17, no. 16, pp. 211-236, (ISBN 0080419208)
    Details
    Publication Date: 1967
    Keywords: Inversion
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Convection and stress propagation in the upper mantle (1967)
    Wiley
    In:  Professional Paper, The Application of Modern Physics to the Earth and Planetary Interiors, New York, Wiley, vol. 9, no. 16, pp. 223-246, (ISBN 1-4020-1729-4)
    Details
    Publication Date: 1967
    Keywords: Stress ; Tectonics ; Inelastic
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Die Lösung linearer Gleichungen nach der Methode der konjugierten Gradienten (1967)
    Wiley
    In:  Mathematische Methoden für Digitalrechner, Sapporo, Japan, Wiley, vol. 1, no. 16, pp. 106-126, (ISBN 0080419208)
    Details
    Publication Date: 1967
    Keywords: Inversion
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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    Friction and Wear of Materials (1965)
    Wiley
    In:  New York, Wiley, vol. 7, no. Publ. No. 12, pp. 127, (ISBN 3-540-44363-0)
    Details
    Publication Date: 1965
    Keywords: Friction ; Physical properties of rocks ; Rock mechanics ; Textbook of geophysics
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    BIBLIOGRAPHY SEISMOLOGY
  • 6
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    An evaluation of the U234/U238 method as a tool for dating pelagic sediments (1965)
    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research, 70 (14). pp. 3457-3474.
    Details
    Publication Date: 2017-12-21
    Description: The possibility of using the 15% excess U234 activity in oceanic uranium for dating pelagic sediments in the age range 100,000 years to more than 1 m.y. has been explored. Results from a series of analyses of bulk samples, mechanical separates, and acid leach fractions indicate that separation of authigenic uranium from detrital uranium by either mechanical or chemical means is impractical. Measurements on totally dissolved samples reveal that the sediments do not form a closed system; post-depositional migration of U234 in the sedimentary column takes place. Based on the experimental data obtained from three red-clay cores with sedimentation rates ranging from 2 to 6 mm/1000 yr, a model depicting diffusion of the U234 generated within the sediments is proposed. The diffusion equation includes three parameters: sedimentation rate, diffusion coefficient for U234, and fraction of the internally produced U234 subject to mobility. If the amount of U234 lost from these cores is typical, a sizeable part of the U234 excess in the sea must be from this source.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
  • 7
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    A hypothesis concerning cyclic flow of salt water related to geothermal heating in the Floridan aquifer (1965)
    Wiley
    In:  Transactions of the New York Academy of Sciences, 28 (2). pp. 249-271.
    Details
    Publication Date: 2020-05-04
    Description: This paper summarizes the hydrogeology of the thick carbonate-evaporite sequence that extends from land surface to the oil horizons at depths of about 11,500 feet below sea level in southern Florida. It sets forth the few known facts about the hydrology of the deep water-bearing rocks and discusses a hypothesis concerning the cyclic flow of salt water related to geothermal heating in the Floridan aquifer. Meinzer (1923, p. 30) defined an aquifer as a "formation, a group of formations, or part of a formation that is water bearing." The connotation of quantity was included by the statement: "Few if any formations are entirely devoid of gravity ground water, but those that do not contain enough to be of consequence as a source of supply are not rated as water bearing." The quality of the water does not enter the definition, for if it did, a change in quality (as by salt-water encroachment) would correspondingly convert aquifers to nonaquifers. This paper treats permeable water-bearing beds as aquifers even though the contained water might be a brine seven times as salty as sea water and, therefore, normally not considered a source of supply.
    Type: Article , PeerReviewed
    Format: text
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    PAPER (OCEANREP)
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