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Browsing by Author "Gose, W. A."

Browsing by Author "Gose, W. A."

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  • Magnetic properties and granulometry of metallic iron in lunar breccia 14313 
    Dunlop, D. J.; Gose, W. A.; Pearce, G. W.; Strangway, David W. (Pergamon Press, 1973)
    Based on a detailed study of time-dependent or viscous remanence (VRM), thermoremanence (TRM) and magnetic granulometry of soil breccia 14313, single-domain particles of iron 100-200 Å in size are proposed as the major ...
  • Magnetic properties of Apollo 14 breccias and their correlation with metamorphism 
    Gose, W. A.; Pearce, G. W.; Strangway, David W.; Larson, E. E. (Pergamon Press, 1972)
    The magnetic properties of Apollo 14 breccias can be explained in terms of the grain size distribution of the interstitial iron which is directly related to the metamorphic grade of the sample.
  • Magnetic properties of Apollo samples and implications for regolith formation 
    Pearce, G. W.; Strangway, David W.; Gose, W. A. (Pergamon Press, 1974)
    The magnetic properties of a number of Apollo 17 samples have been measured and confirm that regoliths of mare sites (Apollo 11, 12, 15 valley, and 17 valley) differ markedly from those of highland sites (Apollo 14, 16, ...
  • Magnetic studies on Apollo 15 and 16 lunar samples 
    Pearce, G. W.; Gose, W. A.; Strangway, David W. (Pergamon Press, 1973)
    The magnetic properties of lunar samples are almost exclusively due to rather pure metallic iron. The mare basalt contains about 0.06 wt.% Fe, the soils 0.5--0.6 wt.%, and the breccias 0.3-1.0 wt.%. Most of the additional ...
  • Remanent magnetization of the lunar surface 
    Pearce, G. W.; Strangway, David W.; Gose, W. A. (Pergamon Press, 1972)
    Two lines of evidence support each other in suggesting that a large volume of the rocks near the lunar surface possess a uniform remanent magnetization with an intensity of about 2 x 10- 6 emu/g. The first line is the ...

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