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  • Dislocation
  • Plate tectonics
  • 1980-1984  (170)
  • 1970-1974  (92)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 122 (1984), S. 560-582 
    ISSN: 1420-9136
    Keywords: Water level ; Fault creep ; Pore pressure ; Dislocation ; Deformation ; Diffusion
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Water-well-level fluctuations associated with episodic creep are studied using a coupled deformation-diffusion solution for the pore pressure produced by a plane-strain shear dislocation moving steadily at a speedV in a linear elastic, saturated porous medium. For largeVr/2c, wherer is distance from the dislocation andc is diffusivity, the solution approaches the form of the uncoupled elastic solution used by Wesson (1981) to analyze water-level changes due to creep events. The differences between the two solutions are significant within 10 diffusion lengths (20c/V) from the fault plane. More specifically, the pore pressure predicted by the coupled solution reverses sign behind the dislocation and is much smaller in magnitude than that predicted by the uncoupled solution. For an undrained Poisson ratio of 0.3, Skempton's coefficient of 0.8 and a shear modulus of 30 GPa, the coupled solution predicts a peak pore-pressure change of 13.7 kPa (137 mbar) per millimeter of slip forV=1 km/day andc=1.0 m2/sec. The spectrum of the coupled solution is limited to a band of frequencies, centered at a value proportional toV and approximately inversely proportional to the distance from the observation point to the fault plant. Thus, close to the fault plane the frequency band occupied by the coupled solution may lie above the range at which water wells can respond. The coupled solution is used in interpreting the same creep-associated water-level change observed by Johnson (1973) and modeled by Wesson (1981) using the uncoupled solution. Although there are uncertainties in properties of the rock material and in the speed of the creep event, the coupled solution predicts a water-level change comparable in magnitude to the observed change.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 6 (1970), S. 11-19 
    ISSN: 1432-0827
    Keywords: Dislocation ; Calcite ; Protein ; Laminar ; Shell
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé Le coquille secondaire (interne) de la valve brachiale deCrania est composée de plaquettes (lamelles) de calcite, séparées l'une de l'autre par des membranes protéiques et formant une succession régulière de couches organiques et inorganiques. Une telle série n'est pas formée couche par couche, l'une aprés l'autre. Au contraire, les lamelles se développent latéralement, généralement à plus d'un niveau, par accroissement dans un liquide extrapallial le long des côtes définis par des dislocations hélicoidales. Simultanément, les membranes protéiques sont déposées dans le même liquide extrapallial sur les surfaces des lamelles en voie de développement, de sorte que non seulement elles sont continues l'une avec l'autre, mais encore elles passent d'un, niveau à l'autre de facon spiralée le long de lignes de dislocation. Les cellules épithéliales, qui sécrètent le liquide extrapallial, sont attachées aux membranes protéiques par des desmosomes, mais ceux-ci peuvent être rompus au fur et à mesure de la migration des centres de déposition par rapport auxmembranes cytoplasmiques des allules sécrétantes.
    Abstract: Zusammenfassung Die sekundäre (innere) Schale der brachialen Klappe vonCrania besteht aus Calcitplättchen (Laminae), die voneinander durch Proteinblätter getrennt sind und eine regelmäßige Folge von abwechslungsweise organischen und anorganischen Schichten bilden.Die Ablagerung erfolgt nicht schichtweise, sondern die Plättchen wachsen seitlich, meistens auf mehreren Ebenen, durch Zuwachs aus einer extrapallialen Flüssigkeit entlang den Kanten, die durch spiralförmige Verschiebungen gekennzeichnet sind. Gleichzeitig wird Protein aus derselben extrapallialen Flüssigkeit ausgeschieden; daraus entstehen an der Oberfläche der sich ausdehnenden Laminae Proteinblätter, welche nicht nur zusammenhängend sind, sondern im allgemeinen sich auch von einer Ebene auf die nächste ausdehnen, indem sie sich spiralförmig um die Verschiebungslinie legen. Äußere Epithelialzellen, welche die extrapalliale Flüssigkeit sezernieren, werden den Proteinblättern mittels Protoplasmabrücken angefügt, die letzteren können jedoch zerstört werden, da im Zusammenhang mit den Plasmalemma der sezernierenden Zellen die Ablagerungszentren verschoben werden.
    Notes: Abstract The secondary (inner) shell of the brachial valve ofCrania is composed of tablets (laminae) of calcite separated from one another by protein sheets and forming a regular succession of alternating organic and inorganic layers. The succession is not deposited in sequence layer by layer. Instead the laminae grow laterally, usually at more than one level, by accretion from an extrapallial fluid along edges defined by screw dislocation. Simultaneously protein is exuded from the same extrapallial fluid to form sheets on the surfaces of the expanding laminae so that the protein sheets not only are continuous with one another but also generally pass from one level to the next spirally around dislocation lines. Outer epithelial cells secreting the extrapallial fluid are attached to the protein sheets by desmosomal connections, but these can be broken as centres of deposition shift around in relationship to the plasmalemmas of the secreting cells.
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  • 3
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    In:  Geology, Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 10, no. 4, pp. 179-185, pp. 2121
    Publication Date: 1982
    Keywords: Seismology ; Teleseismic events ; Body waves ; P-waves ; Shear waves ; earth mantle ; Tectonics ; Plate tectonics ; Subduction zone ; China
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  • 4
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    In:  J. of Geology, Washington D.C., Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 91, no. 1-2, pp. 307-321, pp. L08305
    Publication Date: 1983
    Keywords: Plate tectonics ; Geol. aspects ; Fault zone
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  • 5
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    In:  J. Geophys. Res., Beijing, Pergamon, vol. 76, no. 17, pp. 2674-2689, pp. 2135
    Publication Date: 1971
    Keywords: Tectonics ; Plate tectonics ; JGR
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  • 6
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    In:  J. Geophys. Res., Paris, Pergamon, vol. 89, no. 9, pp. 2425-2443, pp. 1246
    Publication Date: 1984
    Keywords: Plate tectonics ; Seismicity ; Fault plane solution, focal mechanism ; Seismology ; Nabelek ; JGR
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  • 7
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    In:  Geophys. J. R. astr. Soc., Taipei, Elsevier, vol. 75, no. 7, pp. 143-154, pp. 2091, (ISBN: 0-12-018847-3)
    Publication Date: 1983
    Keywords: Earthquake barriers ; Dislocation ; Plate tectonics ; GJRaS
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  • 8
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    In:  Bull. Seism. Soc. Am., Luxembourg, Conseil de l'Europe, vol. 64, no. 8, pp. 555-570, pp. L15S17, (ISBN: 0-12-018847-3)
    Publication Date: 1974
    Keywords: Earthquake ; Fault zone ; Dislocation ; BSSA
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  • 9
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    In:  J. Geophys. Res., Leipzig, Birkhäuser Verlag, vol. 78, no. 4, pp. 7727-7732, pp. 2458, (ISBN: 0-12-018847-3)
    Publication Date: 1973
    Keywords: Seismology ; Dynamic ; Dislocation ; Inelastic ; JGR
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  • 10
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    In:  J. Geophys. Res., Heidelberg, North Holland Publishing Company, vol. 85, no. 4, pp. 3131-3150, pp. 1516, (ISBN: 0-12-018847-3)
    Publication Date: 1980
    Keywords: Dislocation ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Stress ; Inelastic ; JGR
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