Skip to main content
Log in

Megaturbidite: An acceptable term?

  • Published:
Geo-Marine Letters Aims and scope Submit manuscript

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.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  1. Mutti E (1979) Turbidités et cones sous-marins profonds. In: Homewood P (ed) Sédimentation Détrique (Fluviatile, Littorale et Marine). Institute of Geology, Université de Fribourg, pp 353–419

  2. Shanmugam G, Moiola RJ (1985) Submarine fan models: problems and solutions. In: Bouma AH, Normark WR, Barnes NE (eds) Submarine Fans and Related Turbidite Systems. Springer-Verlag, New York, pp 29–34

    Google Scholar 

  3. Mutti E, Ricci Lucchi F, Seguret M, Zanzucchi G (1984) Seismoturbidites; a new group of resedimented deposits. Marine Geology 55:103–116

    Google Scholar 

  4. Hampton MA (1975) Competence of fine-grained debris flows. Journal Sedimentary Petrology 45:834–844

    Google Scholar 

  5. Postma G (1986) Classification for sediment gravity-flow deposits based on flow conditions during sedimentation. Geology 14:291–294

    Google Scholar 

  6. Middleton GV, Hampton MA (1973) Sediment gravity flows: mechanisms of flow and deposition. In: Middleton GV, Bouma AH (eds) Turbidites and Deep-Water Sedimentation. Society of Economic Paleontologists and Mineralogists, Pacific Section, Short Course Lecture Notes (Anaheim, May 12, 1973), pp 1–38

  7. Lowe DR (1979) Sediment gravity flows: their classification and some problems of application to natural flows and deposits. In: Doyle LJ, Pilkey OH (eds) The Geology of Continental Slopes. Society of Economic Paleontologists and Mineralogists Spec. Publ. 27, pp 75–82

  8. Lowe DR (1982) Sediment gravity flows: II, Depositional models with special reference to the deposits of high-density turbidity currents. Journal Sedimentary Petrology 52:279–297

    Google Scholar 

  9. Dzulynski S, Ksiazkiewicz M, Kuenen PH (1959) Turbidites in Flysch of the Polish Carpathian Mountains. Geological Society of American Bulletin 70:1089–1118

    Google Scholar 

  10. Mutti E, Rosell J, Allen G, Fonnesu F, Sgavetti M (1985) The Eocene Baronia tide dominated delta-shelf system in the Ager Basin. International Association Sedimentologists Regional Meeting, Lleida, Spain, Excursion No. 12:579–600

  11. Parea GC, Ricci Lucchi F (1975) Turbidite key beds as indicators of ancient deep sea plains. Proceedings IX Congress International Association Sedimentology, Nice, France, Theme 1:235–242

    Google Scholar 

  12. Ricci Lucchi F (1985) Marnoso-Arenacea turbidite system, Italy. In: Bouma AH, Normark WR, Barnes NE (eds) Submarine Fans and Related Turbidite Systems. Springer-Verlag, New York, pp 209–216

    Google Scholar 

  13. Mutti E, Ricci Lucchi, F (1975) Turbidite facies and facies associations. In: Mutti E, Parea GC, Ricci Lucchi F, Sagri M, Zanzucchi G, Ghibaudo G, Iaccarino S, (eds) Guide Book Field Trip All, IX Congress International Association Sedimentology, Nice, France, pp 21–36

  14. Mutti E, Ricci Lucchi F (1972) Le torbiditi dell' Appennino settentrionale: introduzione all' analisi di facies. Memorie Societa Geologia Italiana 11:161–199

    Google Scholar 

  15. Mutti E (1977) Distinctive thin-bedded turbidite facies and related depositional environments in the Eocene Hecho Group (south-central Pyrenees, Spain). Sedimentology 24:106–131

    Google Scholar 

  16. Mutti E (1985) Turbidite systems and their relations to depositional sequences. In: Zuffa GG (ed) Provenance of Arenites. D Reidel Publishing Co., Dordrecht, pp 65–93

    Google Scholar 

  17. Mutti E, Remacha E, Sgavetti M, Rosell J, Valloni R, Zamorano M (1985) Stratigraphy and facies characteristics of the Eocene Hecho Group turbidite systems, south-central Pyrenees. International Association of Sedimentologists Regional Meeting, Lleida, Spain, Excursion No. 12:531–576

  18. Johns DR, Matti E, Rosell J, Seguret M, (1981) Origin of a thick redeposited carbonate bed in Eocene turbidites of the Hecho Group, south-central Pyrenees, Spain. Geology 9:161–164

    Google Scholar 

  19. Labaume P, Mufti E, Seguret M, Rosell J (1983) Mégaturbidites carbonatées du bassin turbiditique de l'Éocène inférieur et moyen sud-Pyrénéen. Bulletin Societé Geologie, France, XXV:927–941

    Google Scholar 

  20. Labaume P, Seguret M, Mutti E (1986) Calcareous megaturbidites of Eocene South Pyrenean foreland basin. American Association Petroleum Geologists Bulletin 70:609

    Google Scholar 

  21. Puigdefabregas C (1986) Megaturbidites from Eocene of Southern Pyrenees: alternative interpretation. American Association Petroleum Geologists Bulletin 70:635–636

    Google Scholar 

  22. Bourrouilh R, Offroy B (1983) Séquences de mass-flow évolutif-mégaturbidites du flysch sénonien nord-pyrénéen, traitement statistique et anotomie du bassin Sénonien. Geologie Mediterranéenne X:345–359

    Google Scholar 

  23. Bourrouilh R, Coumes F, Offroy B (1984) Méchanismes séquentiels et événements exceptionnels du flysch nord-pyrénéen; correlations par les dépôts gravitaires profonds. Bulletin Societé Geologie, France, XXVI:1223–1234

    Google Scholar 

  24. Rosell J, Remacha E, Zamorano M, Gabaldon V (1985) Estratigrafía de la cuenca turbidítica terciaria de Guipúzcoa; comparación con la cuenca turbidítica prepirenaica central. Boletin Geologico y Minero XCVI-V:471–482

    Google Scholar 

  25. Rosell J, Remacha E, Zamorano M, Gabaldon V (1985) Serie turbidítica del Cretácico Superior del País Vasco. Boletin Geologico y Minero XCVI-V:361–366

    Google Scholar 

  26. Bouma AH, Coleman JM, DSDP Leg 96 Shipboard Scientists (1985) Mississippi Fan: Leg 96 program and principal results. In: Bouma AH, Normark WR, Barnes NE (eds) Submarine Fans and Related Turbidite Systems. Springer-Verlag, New York, pp 247–252

    Google Scholar 

  27. Ward RF, Kendall CG St C, Harris PM (1986) Upper Permian (Guadalupian) facies and their association with hydrocarbons-Permian Basin, West Texas and New Mexico. American Association Petroleum Geologists Bulletin 70:239–262

    Google Scholar 

  28. Elmore RD, Pilkey OH, Cleary WJ, Curran HA (1979) Black shell turbidite, Hatteras Abyssal Plain, western Atlantic Ocean. Geological Society American Bulletin 90:1165–1176

    Google Scholar 

  29. Crevello PD, Schlager W (1980) Carbonate debris sheets and turbidites, Exuma Sound, Bahamas. Journal Sedimentary Petrology 50:1121–1148

    Google Scholar 

  30. Brooks GR, Doyle LJ, McNeillic JI (1986) A massive carbonate gravity-flow deposit intercalated in the lower Mississippi Fan. In: Bouma AH, Coleman JM, Meyer AA, and others, Initial Reports of the Deep Sea Drilling Project Leg 96. US Government Printing Office. Washington, DC, pp 541–546

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Bouma, A.H. Megaturbidite: An acceptable term?. Geo-Marine Letters 7, 63–67 (1987). https://doi.org/10.1007/BF02237985

Download citation

  • Received:

  • Revised:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02237985

Keywords

Navigation