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Carbonates and Evaporites

, Volume 2, Issue 2, pp 89–93 | Cite as

Seismic response to an evaporite/carbonate association

  • Malcolm K. Jenyon
Articles

Abstract

The seismic response to a stratigraphic assemblage including evaporite and carbonate units can be very complex. This is not surprising when such factors are considered as the possible range of rock densities and seismic velocities in the various lithologic units, together with the variety of rock fabrics, solubilities and deformational effects often to be found within such an association. This brief study illustrates examples from the Zechstein evaporite basin of the southern North Sea, and comments on the possible geological and geophysical significance of some of the features that emerge from the detailed seismic response.

In order to put these examples into their geophysical context, a brief discussion of some basic ideas on seismic wave propagation is presented.

Keywords

Halite Anhydrite Evaporite Seismic Response Seismic Velocity 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. ANDERSON, R.Y., & KIRKLAND, D.W., 1980, Dissolution of salt deposits by brine density flow: Geology, v. 8, 66–69.CrossRefGoogle Scholar
  2. JENYON, M.K., CRESSWELL, P.M., & TAYLOR, J.C.M., 1984, Nature of the connection between the northern and southern Zechstein Basins across the Mid North Sea High: Marine & Petroleum Geol. v. 1, 355–363.CrossRefGoogle Scholar
  3. JENYON, M.K., 1986, Salt Tectonics. Elsevier, Barking, U.K., 191pp.Google Scholar
  4. TAYLOR, J.C.M., 1986, Late Permian-Zechstein,in Glennie, K.W. (ed.), Introduction to the Petroleum Geology of the North Sea (2nd. Ed.). Blackwell, Oxford. 236pp.Google Scholar

Copyright information

© Springer 1988

Authors and Affiliations

  • Malcolm K. Jenyon
    • 1
  1. 1.Seismograph Service (England) LimitedKestonEngland

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