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  • (E)-3-tridecen-2-one  (1)
  • Key words: SKS splitting, asthenosphere, plate motion, dislocation-diffusion transition.  (1)
  • 1
    Digitale Medien
    Digitale Medien
    (E)-3-tridecen-2-one, an antibiotic from the interdigital glands of black-tailed deerOdocoileus hemionus columbianus (1995)
    Springer
    Cellular and molecular life sciences 51 (1995), S. 368-369 
    Details
    ISSN: 1420-9071
    Schlagwort(e): Black-tailed deer ; Odocoileus hemionus columbianus ; (E)-3-tridecen-2-one ; antimicrobial activity ; interdigital gland
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Biologie , Medizin
    Notizen: Abstract (E)-3-tridecen-2-one, the major volatile component of interdigital gland extracts from the black-tailed deer,Odocoileus hemionus columbianus, inhibited the growth of gram-positive bacteria and fungi. The bacteria,Propionibacterium acnes, and the fungi,Trichophyton mentagrophytes had a minimum inhibitory concentration (MIC) of 12.5 μg/mL and 25 μg/mL, respectively.
    Materialart: Digitale Medien
    URL: http://dx.doi.org/10.1007/BF01928897
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 2
    Digitale Medien
    Digitale Medien
    On Presence of Seismic Anisotropy in the Asthenosphere beneath Continents and its Dependence on Plate Velocity: Significance of Reference Frame Selection (1998)
    Springer
    Pure and applied geophysics 151 (1998), S. 281-303 
    Details
    ISSN: 1420-9136
    Schlagwort(e): Key words: SKS splitting, asthenosphere, plate motion, dislocation-diffusion transition.
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie , Physik
    Notizen: Abstract —We examine the possibility of seismic anisotropy in the asthenosphere due to present plate motion using SKS splitting results. The fast directions of anisotropy correlate weakly with the directions of the absolute plate motion (APM) for all APM models. Weak correlation indicates the possibility of asthenospheric anisotropy as well as frozen anisotropy in the lithosphere. Detection of strain rate dependence of anisotropy is helpful to further conclusion of the problem. The selection of reference frame is important to describe shear deformation in the asthenosphere beneath continent due to plate motion. The behavior of hot spots to the mesosphere, fixed or drifted by mantle return flow, is a key of the selection of the reference frame. For the NNR-NUVEL1 model, APM correlated anisotropy appears only at plate velocity faster than 1.4 cm/yr. It suggests the new possibility of the formation of asthenospheric anisotropy in addition to frozen anisotropy in the lithosphere. A critical plate velocity for the formation of anisotropy can be caused by the dislocation-diffusion transition as a function of strain rate on a deformation mechanism map of the upper mantle olivine.
    Materialart: Digitale Medien
    URL: http://dx.doi.org/10.1007/s000240050115
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