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  • Other Sources  (4)
  • Oxford Univ. Press  (2)
  • AAPG (American Association of Petroleum Geologists)  (1)
  • AGU  (1)
  • 1960-1964  (4)
  • 1945-1949
  • 1
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    Oxford Univ. Press
    In:  Oxford, Oxford Univ. Press, vol. 3, pp. 158, (ISBN 0-444-50968-2)
    Publication Date: 1964
    Keywords: Textbook of physics ; Friction ; Physical properties of rocks ; Fluids
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  • 2
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    AAPG (American Association of Petroleum Geologists)
    In:  In: Classification of Carbonate Rocks — A Symposium. , ed. by Ham , W. E. AAPG Memoir, 1 . AAPG (American Association of Petroleum Geologists), Tulsa, Oklahoma, pp. 108-121. ISBN 9781629812366
    Publication Date: 2021-01-27
    Description: Three textural features seem especially useful in classifying those carbonate rocks that retain their depositional texture (1) Presence or absence of carbonate mud, which differentiates muddy carbonate from grainstone; (2) abundance of grains, which allows muddy carbonates to be subdivided into mudstone, wackestone, and packstone; and (3) presence of signs of binding during deposition, which characterizes boundstone. The distinction between grain-support and mud-support differentiates packstone from wackestone—packstone is full of its particular mixture of grains, wackestone is not. Rocks retaining too little of their depositional texture to be classified are set aside as crystalline carbonates.
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 3
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    Oxford Univ. Press
    In:  Oxford, 3rd Edition, 459 pp., Oxford Univ. Press, vol. 46, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Publication Date: 1961
    Keywords: Textbook of mathematics ; Statistical investigations ; Error analysis ; Earthquake hazard
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  • 4
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    AGU
    In:  Journal of Geophysical Research, 65 (5). pp. 1535-1541.
    Publication Date: 2020-07-23
    Description: As a part of the measurement of heat flow through the ocean floor, the thermal conductivities of samples of sediment from the Pacific, Atlantic, and Mediterranean areas have been determined in the laboratory by a steady-state method. Average values over a wide range of water content are found to depend more on water content than on solid phase constituents, and conductivities can be read from a diagram if the amount of contained sea water or the wet density of the sediment is known. A graph is included, showing the conductivities of wet, granular materials other than ocean sediment.
    Type: Article , PeerReviewed
    Format: text
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