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  • 1
    Electronic Resource
    Electronic Resource
    Book reviews (1990)
    Springer
    Geo-marine letters 10 (1990), S. 173-175 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02085933
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    Mississippi Fan: Internal structure and depositional processes (1984)
    Springer
    Geo-marine letters 3 (1984), S. 147-153 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Mississippi Fan is a Quarternary accumulation composed of more than seven elongated fan lobes. Isopach and structure maps show frequent shifting of these lobes. The Mississippi Canyon, formed by retrogressive slumping, connects to the youngest fan lobe. The upper fan-lobe is characterized by a large, incised, partially infilled, leveed channel. The middle fan-lobe is aggradational, convex in cross section, with a channel-levee complex on its apex. The lower fan-lobe contains a recently active small channel and several abandoned ones. Depositional patterns can be explained by several processes: “fluvial,” debris flows, and turbidity currents.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02462460
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    Paper (German National Licenses)
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  • 3
    Electronic Resource
    Electronic Resource
    Megaturbidite: An acceptable term? (1987)
    Springer
    Geo-marine letters 7 (1987), S. 63-67 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Terminology should facilitate communication; however, inaccuracies can lead to misunderstanding; new and revived terms normally add to the confusion. Megaturbidite is a rather common term in Europe used to identify a thick, extensive deposit from an exceptionally large mass flow. Their grain size can vary from large blocks to clay size. If the term megaturbidite is used, is should be restricted to layers that: (1) are thick compared to the host rock; (2) are laterally extensive; (3) differ in composition from the host rock; and (4) lack submarine fan geometries. They are excellent markers for stratigraphic and seismic correlations, and useful in basin analyses.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02237985
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    Paper (German National Licenses)
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  • 4
    Electronic Resource
    Electronic Resource
    Editorial announcement (1993)
    Springer
    Geo-marine letters 13 (1993), S. 1-1 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01204385
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    Paper (German National Licenses)
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  • 5
    Electronic Resource
    Electronic Resource
    Book reviews (1986)
    Springer
    Geo-marine letters 6 (1986), S. 57-61 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02311697
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    Paper (German National Licenses)
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  • 6
    Electronic Resource
    Electronic Resource
    Depositional sequences in clastic continental slope deposits, Gulf of Mexico (1981)
    Springer
    Geo-marine letters 1 (1981), S. 115-121 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Tertiary and Quaternary sediments, overlying diapiric older Tertiary shales and Louann Salt on the continental slope in the western Gulf of Mexico, show cyclicity based on seismic-reflection patterns. A set of indistinct parallel reflections or an acoustically semi-transparent zone, normally onlapping onto diapir flanks, alternates with a set of distinct parallel reflections that drape the sea bottom. The indistinct reflections represent deposits employed by bottom transport during a lowering of sea level. Sea level rise and hight stand are characterized by hemipelagic sediments that form blanket-type deposits. Differential sediment loading causes diapiric activity that may reach maximum upward velocities when sea level rises.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02463328
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  • 7
    Electronic Resource
    Electronic Resource
    Editorial (1990)
    Springer
    Geo-marine letters 10 (1990), S. 1-4 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02431015
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    Paper (German National Licenses)
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  • 8
    Electronic Resource
    Electronic Resource
    Northern Gulf of Mexico continental slope (1990)
    Springer
    Geo-marine letters 10 (1990), S. 177-181 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The hummocky continental slope in the northwestern Gulf of Mexico is the result of active salt tectonism and accompanying faulting. Fluid and gassy hydrocarbons rise through the sediment column and along faults causing the formation of gas hydrates, gassy sediments, mud volcanoes and mounds, chemosynthetic communities and authigenic carbonates, reefs, and hardgrounds. Salt activity coupled with processes associated with relative sea level fluctuations create a feedback relationship resulting in the above-mentioned phenomena as well as others such as seafloor erosion at great water depths.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02431064
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    Paper (German National Licenses)
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  • 9
    Electronic Resource
    Electronic Resource
    Book reviews (1992)
    Springer
    Geo-marine letters 12 (1992), S. 187-188 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02084931
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    Paper (German National Licenses)
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  • 10
    Electronic Resource
    Electronic Resource
    Influence of relative sea level changes on the construction of the Mississippi Fan (1989)
    Springer
    Geo-marine letters 9 (1989), S. 161-170 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A conceptual sea-level-driven depositional model for individual fanlobes (channel-overbank systems) of the Mississippi Fan does not permit direct application of the sequence stratigraphic principles of Vail and colleagues. Deep Sea Drilling Project Leg 96 results suggest that, during initial relative lowering of sea level, the canyon and upper fan channel were formed; excavated fine-grained slope sediments may have formed a debris flow deposit base for the fanlobe. Continued lowering produced constructional channel-levee-overbank deposits. Rising relative sea level inhibited input of coarse clastics, and channel depressions filled with muds. A blanket of (hemi)pelagics represents relative high sea level stand.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02431043
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