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  • Weitere Quellen  (7)
  • American Geophysical Union
  • Cell Press
  • Nature Publishing Group (NPG)
  • 1975-1979  (1)
  • 1970-1974  (6)
  • 1
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    Unbekannt
    Effect of water on the experimental deformation of olivine (1972)
    American Geophysical Union
    In:  Professional Paper, Flow and Fracture of Rocks, Washington, D. C., American Geophysical Union, vol. 16, no. 16, pp. 109-115, (ISBN 0080419208)
    Details
    Publikationsdatum: 1972
    Schlagwort(e): Fluids ; Physical properties of rocks ; Laboratory measurements ; Rock mechanics
    Standort Signatur Erwartet Verfügbarkeit
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    BIBLIOGRAFIE SEISMOLOGIE
  • 2
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    Unbekannt
    Seismic anisotropy, flow, and constitution of the upper mantle (1972)
    American Geophysical Union
    In:  Professional Paper, Flow and Fracture of Rocks, Washington, D. C., American Geophysical Union, vol. 16, no. 16, pp. 167-190, (ISBN 1-86239-165-3, vi + 330 pp.)
    Details
    Publikationsdatum: 1972
    Schlagwort(e): Physical properties of rocks ; Seismology ; Anisotropy ; earth mantle ; ConvolutionE
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 3
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    Unbekannt
    Pore pressure in geophysics (1972)
    American Geophysical Union
    In:  Professional Paper, Flow and Fracture of Rocks, Washington, D. C., American Geophysical Union, vol. 16, no. 16, pp. 265-273, (ISBN 0080419208)
    Details
    Publikationsdatum: 1972
    Schlagwort(e): Fluids ; Physical properties of rocks ; Rock mechanics ; Laboratory measurements
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 4
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    Unbekannt
    Deformation of non-Newtonian materials in simple shear (1972)
    American Geophysical Union
    In:  Bull., Polar Proj. OP-O3A4, Flow and Fracture of Rocks, Washington, D. C., American Geophysical Union, vol. 16, no. XVI:, pp. 243-258, (ISBN: 3-540-23712-7)
    Details
    Publikationsdatum: 1972
    Schlagwort(e): Rock mechanics ; Laboratory measurements ; Inelastic ; Physical properties of rocks
    Standort Signatur Erwartet Verfügbarkeit
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    BIBLIOGRAFIE SEISMOLOGIE
  • 5
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    Unbekannt
    Plasticity of single crystals of synthetic quartz (1972)
    American Geophysical Union
    In:  Bull., Polar Proj. OP-O3A4, Flow and Fracture of Rocks, Washington, D. C., American Geophysical Union, vol. 16, no. XVI:, pp. 29-53, (ISBN: 3-540-23712-7)
    Details
    Publikationsdatum: 1972
    Schlagwort(e): Rheology ; Physical properties of rocks ; Inelastic ; Laboratory measurements ; Rock mechanics
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
    BIBLIOGRAFIE SEISMOLOGIE
  • 6
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    Model for aftershock occurrence (1972)
    American Geophysical Union
    In:  Bull., Polar Proj. OP-O3A4, Flow and Fracture of Rocks, Washington, D. C., American Geophysical Union, vol. 16, no. 1, pp. 259-263, (ISBN: 3-540-23712-7)
    Details
    Publikationsdatum: 1972
    Schlagwort(e): Modelling ; Aftershocks ; Seismology ; Seismicity
    Standort Signatur Erwartet Verfügbarkeit
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    BIBLIOGRAFIE SEISMOLOGIE
  • 7
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    Phreatomagmatic origin of the olivine melilitite diatremes of the Swabian Alb, Germany (1979)
    American Geophysical Union
    In:  In: Kimberlites, Diatremes, and Diamonds: Their Geology, Petrology, and Geochemistry. , ed. by Boyd, F. R. American Geophysical Union, Boulder, Colorado, USA, pp. 354-363. ISBN 0-87590-212-X
    Details
    Publikationsdatum: 2020-01-28
    Beschreibung: The olivine melilitite diatemes of the Swabian Alb, frequently compared with kimberlite diatremes, are discussed in terms of hydrogeological setting, internal structure and juvenile fraction. The hydrogeological conditions of the Swabian Alb at the time of diatreme emplacement were characterized by copious amounts of groundwater within the sedimentary cover of the basement. Subsequently to the eruptions groundwater accumulated within the maars of the larger diatremes forming fresh‐water lakes as also happened nearby in the Steinheim and Ries impact craters. The diatremes reveal subsidence structures composed of large wall‐rock blocks, subaerially deposited pyroclastic beds, and well‐bedded reworked pyroclastic debris which accumulated on the floor of the fresh‐water crater lakes. The latter fact implies availability of groundwater at the time the diatremes formed. The juvenile fraction is developed in the shape of spherical to ovoid nucleated autoliths of ash to lapilli size that are macroscopically nearly devoid of vesicles. The autoliths are interpreted as the product of water vapor explosions which took place when rising olivine melilitite magma contacted groundwater and was fragmented into magma droplets. The droplets were rapidly chilled and thus preserved their shape. Because of the hydrogeological data, the diatreme structure, and the chilled nature of the autoliths a phreatomagmatic origin of the Swabian diatremes is suggested.
    Materialart: Book chapter , NonPeerReviewed
    Format: text
    Standort Signatur Erwartet Verfügbarkeit
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    ARTIKEL (OCEANREP)
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