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

M. Sonderholm

doi:10.1007/bfb0011376

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

M. Sonderholm

Geological Data Centre

Research output: Chapter in Book/Report/Conference proceeding › Chapter in book › Research › peer-review

1 Citation (Scopus)

Abstract

The Dolomite-Anhydrite Transition Zone is an important marker horizon separating the thick successions of grey halite of the Zechstein 1 and 2 cyles in the central parts of the Norwegian-Danish Basin. Within this unit, six main facies have been recognized. These can be grouped into three facies associations which reflect major events in the evolution of the basin. -from Author

Original language	English
Title of host publication	Lecture Notes in Earth Sciences
Subtitle of host publication	The Zechstein facies in Europe
Editors	Tadeusz M. Peryt
Publisher	Springer
Pages	93-122
Number of pages	30
ISBN (Print)	3540177108
DOIs	https://doi.org/10.1007/bfb0011376
Publication status	Published - 1987

Publication series

Name	Lecture Notes in Earth Sciences: The Zechstein facies in Europe
Publisher	Springer

Programme Area

Programme Area 4: Mineral Resources

Access to Document

10.1007/bfb0011376

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Sonderholm, M. (1987). 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. In T. M. Peryt (Ed.), Lecture Notes in Earth Sciences: The Zechstein facies in Europe (pp. 93-122). (Lecture Notes in Earth Sciences: The Zechstein facies in Europe). Springer. https://doi.org/10.1007/bfb0011376

Sonderholm, M. / 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. Lecture Notes in Earth Sciences: The Zechstein facies in Europe. editor / Tadeusz M. Peryt. Springer, 1987. pp. 93-122 (Lecture Notes in Earth Sciences: The Zechstein facies in Europe).

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abstract = "The Dolomite-Anhydrite Transition Zone is an important marker horizon separating the thick successions of grey halite of the Zechstein 1 and 2 cyles in the central parts of the Norwegian-Danish Basin. Within this unit, six main facies have been recognized. These can be grouped into three facies associations which reflect major events in the evolution of the basin. -from Author",

author = "M. Sonderholm",

year = "1987",

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series = "Lecture Notes in Earth Sciences: The Zechstein facies in Europe",

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Sonderholm, M 1987, 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. in TM Peryt (ed.), Lecture Notes in Earth Sciences: The Zechstein facies in Europe. Lecture Notes in Earth Sciences: The Zechstein facies in Europe, Springer, pp. 93-122. https://doi.org/10.1007/bfb0011376

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. / Sonderholm, M.

Lecture Notes in Earth Sciences: The Zechstein facies in Europe. ed. / Tadeusz M. Peryt. Springer, 1987. p. 93-122 (Lecture Notes in Earth Sciences: The Zechstein facies in Europe).

Research output: Chapter in Book/Report/Conference proceeding › Chapter in book › Research › peer-review

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AB - The Dolomite-Anhydrite Transition Zone is an important marker horizon separating the thick successions of grey halite of the Zechstein 1 and 2 cyles in the central parts of the Norwegian-Danish Basin. Within this unit, six main facies have been recognized. These can be grouped into three facies associations which reflect major events in the evolution of the basin. -from Author

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Sonderholm M. 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. In Peryt TM, editor, Lecture Notes in Earth Sciences: The Zechstein facies in Europe. Springer. 1987. p. 93-122. (Lecture Notes in Earth Sciences: The Zechstein facies in Europe). doi: 10.1007/bfb0011376

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

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