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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: AWI G1-94-0068-4 ; AWI G1-94-0068-1 ; AWI G1-94-0068-2 ; AWI G1-94-0068-3
    Type of Medium: Monograph available for loan
    Pages: XVI, 439 S. : Ill., graph. Darst., Kt.
    ISBN: 3540061150
    Branch Library: AWI Library
    Branch Library: AWI Library
    Branch Library: AWI Library
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 93.0223
    Type of Medium: Monograph available for loan
    Pages: XVI, 439 S. : zahlr. Ill.
    Edition: corr. repr. of the 1. ed.
    ISBN: 3540073779
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Series available for loan
    Series available for loan
    Köln : von Loga
    Associated volumes
    Call number: SR 90.0064(27)
    In: Clausthaler tektonische Hefte
    Type of Medium: Series available for loan
    Pages: 123 S. : graph .Darst.
    ISBN: 3873610272
    Series Statement: Clausthaler tektonische Hefte 27
    Classification: A.3.5.
    Language: German
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 2 (1963), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Sand and clay porosities of foreshore, tidal flat, and shallow sea sediments from the southern North Sea were determined. No definite relationship could be observed between porosity, condensation ratio, and depositional environment.Porosity increases with increasing clay content. The clay porosity probably depends to some degree on the rate of sedimentation. The porosity of experimentally deposited sands increases with decreasing grain size. The same relation can be observed with fossil sandstones. In Recent sands, this increase may be compensated by a closer packing arrangement of the finer grains, expressed by a higher condensation ratio〈displayedItem type="mathematics" xml:id="mu1" numbered="no"〉〈mediaResource alt="image" href="urn:x-wiley:00370746:SED294:SED_294_mu1"/〉(P= natural porosity, Pw and Pd are the porosities of the loosest and closest arrangements under water, respectively).Under certain conditions, the sand(stone) porosity decreases continuously with increasing depth (Fig. 7).
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 11 (1968), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Ripple, flaser and lenticular bedding are well known, but for describing profiles, they are not sufficiently defined and subdivided. It is, therefore, the intent of the following text to present such a definition and classification.The classification contains the following main bedding types and intermediary types (Fig.1):〈inlineGraphic alt="inline image" href="urn:x-wiley:00370746:SED99:SED_99_f1" location="image_n/SED_99_f1.gif"/〉〈list xml:id="l1" style="custom"〉1Cross-bedding with flasers.2Flaser bedding, subdivided in: (a) simple flaser bedding; (b) bifurcated flaser bedding; (c) wavy flaser bedding; (d) bifurcated wavy flaser bedding.3Wavy bedding.4Lenticular bedding with thick or flat lenses, subdivided in: (a) continuous lenticular bedding (with connected lenses); (b) broken lenticular bedding (with single lenses).
    Type of Medium: Electronic Resource
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  • 6
    facet.materialart.
    Unknown
    Schweizerbart Science Publishers
    In:  Senckenbergiana Maritima, 10 (4/6). pp. 213-227.
    Publication Date: 2018-09-04
    Description: The pollution history of the metals iron, chromium, nickel, cobalt, zinc, lead, copper, cadmium, and mercury in a sediment profile from the German Bight (southeastern part of the North Sea; Förstner & Reineck, 1974) has been re-interpreted according to new radiometric age data from 210Pb and 137Cs concentrations. Between two units of relative uniform sedimentation - approx. 18 mm/y at 7-19 cm sediment depth and approx. 16 mm/y for the core section from 28-50 cm - a major hiatus and an interval of abnormally low sedimentation rate has been detected (19-28 cm) indicating that sediments deposited at the beginning of the century are directly covered by the most recent sediments. Contamination by Zn, Pb, Cu, Cd and Hg has increased since the second half of the last century, probably due to higher metal inputs from both fossil fuel burning and sewage effluents. The more recent increase of iron, chromium, nickel, and cobalt is possibly related to the dumping of acid iron waste from titanium oxide production.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    facet.materialart.
    Unknown
    Natur und Museum
    Publication Date: 2017-04-12
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , NonPeerReviewed
    Format: application/pdf
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 56 (1967), S. 420-438 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract A diagram is constructed to show the relationship between physiotope, sediment structures sediment textures and endofauna. In this diagram the differences between subenvironments can be pointed out. It is also possible to compare clastic environments if biological parameters are neglected.
    Abstract: Résumé Un diagramme est construit pour montrer la relation entre le physiotope, les structures sédimentaires, le matériel détritique et l'endofauna. Il est possible de montrer les différences des milieux subaquatiques.
    Notes: Zusammenfassung Es wird eine graphische Darstellung gegeben, aus welcher die Beziehungen zwischen dem Physiotop, den dazugehörenden Sedimenten, deren Gefügen und der Endofauna ersichtlich sind. In dieses Diagramm lassen sich bei äquivalenten biologischen Parametern stufenlos alle Unterbereiche von Ablagerungsräumen darstellen und deren Übereinstimmungen oder Gegensätzlichkeiten aufzeigen. Auch unterschiedliche klastische Ablagerungsbereiche können eingezeichnet und miteinander verglichen werden, wenn die Äquivalenz biologischer Parameter, wie Salzgehalt, Temperatur, Licht, Nahrungsangebot oder O2-Sättigung, vernachlässigt wird.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 49 (1960), S. 149-161 
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Zusammenfassung Zum Begriff „Sedimentations-Geschwindigkeit“ werden zwei Unterbegriffe vorgeschlagen: „Mächtigkeitszunahme“ und „Schichtungs-Geschwindigkeit“. Die Mächtigkeitszunahme errechnet sich aus der Mächtigkeit eines Sedimentkörpers, geteilt durch die Bildungszeit. Die Schichtungs-Geschwindigkeit errechnet sich aus der Mächtigkeit einer Einzelschicht, geteilt durch die Zeit der pausenlosen Bildung dieser Schicht. Mächtigkeitszunahme verglichen mit Schichtungs-Geschwindigkeit ergibt, daß die Schichten in Flachsee-Sedimenten vom Gezeiten-Meer nur den 1/10 000 bis 1/100 000 der Gesamtbildungszeit dokumentieren.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract Thin sandlayers embedded in mud of various depositional sedimentary environments are compared. From a study of their characteristics such as grading, internal structure, size, lateral decrease of grain size and form, conclusions can be drawn about the various sedimentary environments.
    Abstract: Résumé L'auteur compare les minces intercalations sableuses dans les boues, provenant de différents domaines sédimentaires. On peut dès lors en se basant sur différentes caractéristiques, comme le granoclassement, le type structural de la couche, la grandeur, la puissance, la diminution latérale de la granularité et la forme, émettre des conclusions sur le domaine où s'est effectué le dépôt.
    Notes: Zusammenfassung Es wurden dünne, im Schlick eingebettete Sandlagen aus verschiedenen Ablagerungsbereichen verglichen. Dabei können anhand unterschiedlicher Merkmale, wie Gradierung, Art des Schichtgefüges, Größe, Mächtigkeit, laterale Korngrößenabnahme und Form, Schlüsse auf die Ablagerungsbereiche gezogen werden.
    Type of Medium: Electronic Resource
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