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  • 1
    Monograph available for loan
    Monograph available for loan
    Submarine Canyons and other sea valleys (1966)
    Chicago : Rand McNally
    Details Availability
    Call number: M 97.0183
    Type of Medium: Monograph available for loan
    Pages: XIII, 381 S.
    Classification:
    Tectonics
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Submarine geology (1963)
    New York, NY [u.a.] : Harper
    Details Availability
    Call number: G 5525
    Type of Medium: Monograph available for loan
    Pages: XVIII, 557 S. : Ill., graph. Darst., Kt. + 1 Kt.-Beil.
    Edition: 2. ed.
    Series Statement: Harper's geoscience series
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    The Earth beneath the sea (1959)
    Baltimore : Hopkins
    Details Availability
    Call number: G 5563
    Type of Medium: Monograph available for loan
    Pages: XII, 275 S.
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    Our changing coastlines (1971)
    New York, NY [u.a.] : McGraw-Hill
    Details Availability
    Call number: M 94
    Type of Medium: Monograph available for loan
    Pages: 579 S. : Ill.
    Series Statement: An International Oceanographic Foundation Selection
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 5
    Electronic Resource
    Electronic Resource
    Submarine Geology and Geophysics (1940)
    [s.l.] : Nature Publishing Group
    Nature 146 (1940), S. 431-432 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] THE brief article by Dr. Bullard entitled “Geophysical Study of Submarine Geology” which appeared in NATURE of May 18, p. 764, was gratifying in that it directed attention to some of the developments in the newest field of geological research. On the other hand, this article showed a pardonable ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/146431b0
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    Paper (German National Licenses)
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  • 6
    Electronic Resource
    Electronic Resource
    SEDIMENTATION IN SAN DIEGO TROUGH AND CONTRIBUTING SUBMARINE CANYONS (1962)
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 1 (1962), S. 0 
    Details
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: There are a series of basins off southern California, all presumably due to faulting of the broad continental borderland. Of these, San Diego Trough is the only one where sedimentation has gone on sufficiently to fill the basin depressions so that there is a continuous slope southward to where the trough connects with the deeper San Clemente Basin. This deposition has apparently come to a very great extent from turbidity currents moving down submarine canyons developing channeled fans at the canyon bases. All along the canyons and channels as well as across the fans and in San Diego Trough there are sequences of turbidite sands alternating with muddy sediments that represent the normal deep water sedimentation. Comparison of the coarse fraction from the sands and from the interbedded muds shows that the former are predominantly terrigenous in character whereas a large proportion of the latter are biogenous. Mica is quite low in the coarser sand layers but is abundant in the coarse fraction of the muds. Diatoms and radiolarians are largely confined to the mud layers where they may constitute a large percentage of the sand fraction.Study of the heavy and light minerals shows that the sediments of San Diego Trough are derived largely from the nearby land masses rather than having a considerable admixture from the north as would be the case if sediments were being brought down by turbidity currents coming into the trough from the north. The alterites are appa-rently lower in San Diego Trough than in the near shore source area which suggests that a supply of sediments may be picked up from the canyon or channel walls along the way to the trough. Also the finding of the only coarse sands in the middle reaches of the channels suggests local sources as does the general make up of these coarse sands. Despite these locally derived coarse sands the prevalence of very fine sand and the “mud” layers between sand layers suggest that the turbidity currents supplying sediments to San Diego Trough have low velocities or at any rate little erosive capacity.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-3091.1962.tb00029.x
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  • 7
    Electronic Resource
    Electronic Resource
    Sedimentation of the northwestern Gulf of Mexico (1958)
    Springer
    International journal of earth sciences 47 (1958), S. 150-167 
    Details
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Six years of intensive study of the shallow water sediments of the northwestern Gulf of Mexico have indicated that there are many criteria by which ancient sediments deposited under similar conditions can be recognized. Thus the presence of echinoid fragments and of glauconite-filled Foraminifera tests favors marine shelf deposition over bay deposits; calcareous aggregates and grains of gypsum suggest high salinity bay deposits; abundance of wood fibers, high mica content, ferruginous aggregates, and well laminated sediments all are suggestive of deposition near river mouths; greater roundness distinguishes dunes from adjacent beach sands; and coarser grain size distinguishes beach sands from shallow shelf sands in the vicinity. Faunal assemblages of Foraminifera, Ostracoda, and Mollusca all serve to distinguish between bay and shelf deposits. Within the bays the faunas show a close relationship to salinity conditions whereas on the shelf the faunas are arranged in bands parallel to the shore and to the depth contours. Certain generalizations concerning the relation of faunas to environment can be made without detailed knowledge of the species.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01802323
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  • 8
    Electronic Resource
    Electronic Resource
    Pulsating turbidity currents with relationship to high swell and high tides (1975)
    [s.l.] : Nature Publishing Group
    Nature 258 (1975), S. 704-706 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The computerised current meter record showing the times and velocities of upcanyon and downcanyon flows clearly indicates a change in the pattern during the period of high swell. Before and after the large waves, there was an alternation of flows up and down the canyon with velocities not exceeding ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/258704a0
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  • 9
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    Dangerous currents in the surf (1949)
    American Institute of Physics
    Details
    Publication Date: 1949-08-01
    Print ISSN: 0031-9228
    Electronic ISSN: 1945-0699
    Topics: Physics
    Published by American Institute of Physics
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  • 10
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    Tidal Components of Currents in Submarine Canyons (1976)
    University of Chicago Press
    Details
    Publication Date: 1976-05-01
    Print ISSN: 0022-1376
    Electronic ISSN: 1537-5269
    Topics: Geosciences
    Published by University of Chicago Press
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