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  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: SR 90.0002(500-C)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: III, C-14 S.
    Series Statement: U.S. Geological Survey professional paper 500-C
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    In:  Bull. Seism. Soc. Am., Hokkaido University, Pergamon, vol. 47, no. 1-2, pp. 89-110, pp. B10302, (ISSN: 1340-4202)
    Publication Date: 1957
    Keywords: Source ; Seismology ; Fault plane solution, focal mechanism ; BSSA
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  • 3
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    In:  Bull. Seism. Soc. Am., Hokkaido University, Pergamon, vol. 54, no. 1-2, pp. 1519-1528, pp. B10302, (ISSN: 1340-4202)
    Publication Date: 1964
    Keywords: Source ; Seismology ; Fault plane solution, focal mechanism ; BSSA
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  • 4
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    Univ. Toronto Press
    In:  Toronto, 3rd Edition, 353 pp., Univ. Toronto Press, vol. 20, no. Publ. No. 12, pp. 23-40, (ISBN 1-4020-3326-5, VIII + 343 pp.)
    Publication Date: 1974
    Keywords: Textbook of geophysics ; Stress ; Friction ; Fluids ; Physical properties of rocks
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  • 5
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    In:  Bull. Seism. Soc. Am., London, Am. Soc. Mech. Eng., vol. 53, no. 4, pp. 811-816, pp. 2099, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1963
    Keywords: Fault plane solution, focal mechanism ; Statistical investigations ; Earthquake ; Source ; BSSA
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  • 6
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    In:  Bull. Seism. Soc. Am., Taipei, 3-4, vol. 89, no. 5, pp. 1296-1312, pp. 2151, (ISSN: 1340-4202)
    Publication Date: 1999
    Keywords: Seismology ; Source ; Surface waves ; Rayleigh waves ; Earthquake precursor: others (animal behav., wobble, tides) ; Earthquake precursor: prediction research ; BSSA
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  • 7
    ISSN: 1432-0495
    Keywords: Glaciation ; Buried channels ; Canada ; Joints ; Contaminant migration
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The bedrock surface of many glaciated areas is obscured by thick drift deposits. In southern Ontario, Canada, the buried bedrock surface is dissected by channels, infilled with glacial deposits as much as 150 m thick, that are part of a wider mid-continent “preglacial” fluvial system that predates formation of the modern Great Lake basins. The infills of bedrock channels form major groundwater aquifers, influence regional groundwater flows and contaminant migration to Lake Ontario, and may localize the release of thermogenic methane and radon within heavily urbanized surface environments. A quantitative comparison of the regional pattern of bedrock joints and the orientation pattern of buried bedrock channels and modern river valleys shows that all these orientation patterns are virtually coincident. Buried bedrock channels in south-central Ontario are not part of a simple antecedent drainage system but were likely “predesigned” by bedrock joint patterns that have subsequently been propagated upward into overlying Pleistocene sediments. Joints in sediments are of considerable environmental significance (for example, subsurface contaminant and gas migration in fine-grained clayey sediments) and of many origins (stress release, desiccation, etc.) but are widely assumed to be a predominantly surface-related phenomena; the existence of deeper joints has been noted by some authors but their origin is obscure. Data presented herein from south-central Ontario confirm that, in addition to surface-related joints, a second population of bedrock-related joints, reflecting the upward propagation of bedrock fractures, is present in Pleistocene sediments of south-central Ontario.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 41 (1958), S. 101-106 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary The thesis is advanced that hoodoos (mushroom-shaped erosional features in badlands) are caused by water from cloudbursts turning the corner at the brim of the overhang, flowing for a distance upside-down on the underside. This type of upside-down flow is well known as «teapot effect» in the case of tea being poured from a pot flowing down the underside of the spout rather than straight on into the cup. The measured overhang of hoodoos is in good agreement with the theoretical values obtained from hydrodynamic stability considerations.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 52 (1962), S. 69-82 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary The theory of the formation of marine terraces is studied. A model is set up which is believed to describe the physical processes involved. This model leads to a nonlinear partial differential equation which is integrated for some special cases by means of a digital computer. Asymptotic solutions of the differential equation are also found by direct analytical means. It is found that no terraces can develop if eustatic changes occur at a constant rate, contrary to some contentions that have been advanced in the literature.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 89 (1971), S. 32-44 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary This paper discusses a class of stochastic models of flow through porous media in which the randomness is attached to the structure of the medium rather than to the flow path. These models are obtained by generalizing an earlier model available in the literature where a regular ‘crystal’ was taken in which bonds (flow channels) were dammed in a random fashion, yielding a ‘random maze’. The hydraulic properties of general models of this type are calculated; in particular, it is shown that they exhibit the phenomenon of dispersion whereby the factor of dispersion turns out to be a linear function of the percolation velocity.
    Type of Medium: Electronic Resource
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