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  • 1
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    Topics in communication theory (1965)
    McGraw-Hill
    In:  New York, McGraw-Hill, vol. 34, no. 1, pp. 65-66, (ISBN: 3-528-02574-3)
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    Publication Date: 1965
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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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)
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    Publication Date: 1965
    Keywords: Friction ; Physical properties of rocks ; Rock mechanics ; Textbook of geophysics
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    The Fourier Transform and its Applications (1965)
    McGraw-Hill
    In:  New York, McGraw-Hill, vol. 173, pp. 158, (ISBN 0-444-50968-2)
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    Publication Date: 1965
    Keywords: Fourier transform ; Textbook of mathematics
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    BIBLIOGRAPHY SEISMOLOGY
  • 4
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    Probability, Random Variables and Stochastic Processes (1965)
    McGraw-Hill
    In:  New York, McGraw-Hill, vol. 15, no. Publ. No. 12, pp. 585, (ISBN 0080424309)
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    Publication Date: 1965
    Keywords: Statistical investigations ; Handbook of mathematics
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    BIBLIOGRAPHY SEISMOLOGY
  • 5
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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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