The Zechstein Facies in Europe

The Zechstein Facies in Europe edited by Tadeusz M. Peryt.

This book reports new developments in research on the Zechstein basin which is one of the classical saline giants. Recently much information was gathered which changes earlier ideas on the deposition and diagenesis of the Zechstein basin.

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Bibliographic Details
Corporate Author: SpringerLink (Online service)
Other Authors: Peryt, Tadeusz M. (Editor)
Format: eBook
Language:English
Published: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 1987.
Edition:1st ed. 1987.
Series:Lecture Notes in Earth Sciences, 10
Springer eBook Collection.
Subjects:
Sedimentology.
Geology.
Mineralogy.
Geophysics.
Electronic resources (E-books)
Online Access:Click to view e-book
Holy Cross Note:Loaded electronically.
Electronic access restricted to members of the Holy Cross Community.
Table of Contents:
  • Cyclic carbonate and sulphate from the Upper Permian Karstryggen Formation, East Greenland
  • The upper permian (Zechstein) tunstall reef of North East England: Palaeoecology and early diagenesis
  • Dissolution effects and reef-like features in the Zechstein across the Mid North Sea High
  • Regional salt movement effects in the English Southern Zechstein Basin
  • Facies and geochemical aspects of the Dolomite-Anhydrite Transition Zone (Zechstein 1–2) in the Batum-13 well, northern Jutland, Denmark: A key to the evolution of the Norwegian-Danish Basin
  • Sedimentology and facies development of the stassfurt main dolomite in some wells of the South Oldenburg region (Weser-Ems area, NW Germany)
  • The Zechstein sulphates: The state of the art
  • Palaeogeography and sedimentary model of the Kupferschiefer in Poland
  • Sedimentary facies in the Oldest Rock Salt (Na1) of the Leba elevation (northern Poland)
  • The Zechstein (upper permian) Main Dolomite deposits of the Leba elevation, northern Poland: Diagenesis
  • The peritidal sabkha type stromatolites of the platy dolomite (Ca3) of the Leba Elevation (north Poland).

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