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    Contents of Volume 135 – Transaction A.I.M.E., 1939

    Some Things We Don't Know about the Creep of Metals. By H. W. Gillett (T.P. 1087) Reduction of Iron Ores under Pressure by Hydrogen. By Michael Tenenbaum and T. L. Joseph (T.P. loll,

    Jan 1, 1939

  • AIME
    Contents of Volume 135 – Transaction A.I.M.E., 1939

    Some Things We Don't Know about the Creep of Metals. By H. W. Gillett (T.P. 1087) Reduction of Iron Ores under Pressure by Hydrogen. By Michael Tenenbaum and T. L. Joseph (T.P. loll,

    Jan 1, 1939

  • AIME
    Contents of Volume 137 (Institute of Metals Division)

    Page Foreword. By Edmund M. Wise..................... 3 A.I.M.E. Officers and Dircctors...................... 4 Institute of Metals Division Officers and Committees............

    Jan 1, 1940

  • AIME
    Contents of Volume 137 (Institute of Metals Division)

    Page Foreword. By Edmund M. Wise..................... 3 A.I.M.E. Officers and Dircctors...................... 4 Institute of Metals Division Officers and Committees............

    Jan 1, 1940

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    Contents of Volume 150 (Iron and Steel Division)

    Time as a Factor in the Making and Treating of Steel. By John Johnston. (Howe Lecture) (T.P. 1478) Influence of Chromium and Molybdenum on Structure, Hardness and Decarburization of 0.35 Per Cen

    Jan 1, 1942

  • AIME
    Contents of Volume 150 (Iron and Steel Division)

    Time as a Factor in the Making and Treating of Steel. By John Johnston. (Howe Lecture) (T.P. 1478) Influence of Chromium and Molybdenum on Structure, Hardness and Decarburization of 0.35 Per Cen

    Jan 1, 1942

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    Continent-Margin Tectonics And Ore Deposits, Western United States

    By Daniel R. Shawe

    Ore deposits of the western U.S. are divisible broadly into two genetic groups, a smaller one that fits the plate tectonic model of subduction and a larger one that appears unrelated to subduction. So

    Jan 1, 1978

  • IMMS
    Continental Margin Hydrothermal Mineralization: Southern California Borderland

    By James R. Hein

    Barite and Fe-Mn-oxide deposits that occur along faults in the Southern California Borderland formed by low-temperature hydrothermal processes. The Borderland region consists of block-faulted continen

    Jan 1, 2002