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Distinctive Features of Sandy Tempestites

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Cyclic and Event Stratification

Abstract

Sedimentological and biological features allow to distinguish wave-generated storm sands from current-generated sandy turbidites and flood deposits. The origin of some of these features remains still uncertain.

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References

  • AIGNER, T. & FUTTERER, E. 1978: Kolk-Töpfe und -Rinnen (pot and gutter casts) im Muschelkalk-Anzeiger für Wattenmeer? N.Jb.Geol.Paläont., Abh., 156: 285–304.

    Google Scholar 

  • BENDER, F. 1963: Stratigraphie der “Nubischen Sandsteine” in Südjordanien.-Geol.Jb., 81: 237.

    Google Scholar 

  • BLOOS, G. 1976: Untersuchungen über Bau und Entstehung der feinkörnigen Sandsteine des Schwarzen Jura alpha (Hettangium und tiefstes Sinemurium) im schwäbischen Sedimentationsbereich.-Arb.Inst.Geol.Pal.Univ. Stuttgart, N.F. 71.

    Google Scholar 

  • BOUMA, A.H. 1962: Sedimentology of some flysch deposits: A graphic approach to facies interpretation.-Elsevier (Amsterdam).

    Google Scholar 

  • BRENCHLEY, P.J.; NEWALL, G. & SANTSTREET, J.G. 1979: A storm surge origin for sandstone beds in an epicontinental platform sequence, Ordovician, Norway.-Sedim.Geol., 22: 185–217.

    Article  Google Scholar 

  • COOK, D.O. 1970: The occurrence and geologic work of rip currents off Southern California.-Mar. Geol., 9: 173–186.

    Google Scholar 

  • FUCHS, Th. 1895: Studien über Fucoiden und Hieroglyphen.-Denkschr. math. nat. Kl. Akad. Wiss., Wien 62: 369–448.

    Google Scholar 

  • GOLDRING, R. & SEILACHER, A. 1971: Limulid undertracks and their sedimentological implications.-N.Jb.Geol.Paläont., Abh., 137: 422–442.

    Google Scholar 

  • GOLDRING, R. & BRIDGES, P. 1973: Sublittoral sheet sandstones. J. sed. Petr., 43: 736–747.

    Google Scholar 

  • HAMBLIN, A.P., DUKE, W.L. & WALKER, R.G. 1979: Hummocky cross stra- tification-indicator of storm-dominated shallow marine environments.-Am.Ass.Petrol.Geol., Bull. 63: 460–461.

    Google Scholar 

  • HANTZSCHEL, W. & REINECK, H.E. 1968: Faziesuntersuchungen im Hettangium von Helmstedt (Niedersachsen). Mitt. geol. Staatsinst. Hamburg 137: 5–39.

    Google Scholar 

  • KUMAR, N. & SANDERS, J.E. 1978: Storm deposits.-In: FAIRBRIDGE, R.W. & BOURGEOIS (ed.): The encyclopedia of sedimentology.-Encyclop. Earth Sci. Ser., 6: 767–770.

    Google Scholar 

  • MÜLLER, A.H. 1955: Ober die Lebensspur Isopodichnus aus dem Oberen Buntsandstein (Unt.Röt) von Göschwitz bei Jena und Abdrücke ihres mutmaßlichen Erzeugers.-Geologie 4: 481–489.

    Google Scholar 

  • REINECK, H.E. & SINGH,I.B. 1980: Depositional sedimentary environments (2nd. ed). Springer Verl.Berlin, Heidelberg, New York.

    Google Scholar 

  • ROSENKRANZ, D. 1971: Zur Sedimentologie und Ökologie von Echinodermen-Lagerstätten.-N.Jb.Geol.Paläont., Abh., 138: 56–100.

    Google Scholar 

  • SCHMALFUSS, H. 1978: Constructional morphology of cuticular terraces in trilobites, with conclusions on synecological evolution.-N.Jb.Geol.Paläont., Abh., 157: 164–168.

    Google Scholar 

  • SEILACHER, A. 1953: Studien zur Palichnologie. II. Die fossilen Ruhespuren (Cubichnia).-N.Jb.Geol.Paläont., Abh.,98: 87–124

    Google Scholar 

  • SEILACHER, A. 1962: Paleontological studies on turbidite sedimentation and erosion. J.Geol., 70: 227–234

    Article  Google Scholar 

  • SEILACHER, A. 1970: Cruziana stratigraphy of “non-fossiliferous” Palaeozoic sandstones.-In: CRIMES & HARPER (eds.) Trace fossils; Geol. J. Spec. Issue No. 3: 447–476.

    Google Scholar 

  • SEILACHER, A. 1977: Pattern analysis of Paleodictyon and related trace fossils.-In: CRIMES & HARPER (eds.) Trace fossils 2. Geol Spec. Issue No. 9: 289–334.

    Google Scholar 

  • TUNBRIDGE, I.P. 1981: Sandy high-energy flood sedimentation–some criteria for recognition, with an example from the Devonian of S.W. England.-Sedim.Geol., 28: 79–95.

    Article  Google Scholar 

  • WHITTINGTON, H. 1980: Exoskeleton, moult stage, appendage morphology, and habits of the Middle Cambrian trilobite OZenoides serratus. Palaeontology, 23: 171–204.

    Google Scholar 

  • WURSTER, P. 1964: Geologie des Schilfsandsteins.-Mitt. geol. Staatsinst. Hamburg, 33.

    Google Scholar 

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© 1982 Springer

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Seilacher, A. (1982). Distinctive Features of Sandy Tempestites. In: Einsele, G., Seilacher, A. (eds) Cyclic and Event Stratification. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-75829-4_24

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  • DOI: https://doi.org/10.1007/978-3-642-75829-4_24

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-540-11373-7

  • Online ISBN: 978-3-642-75829-4

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