Cyclic carbonate and sulphate from the Upper Permian Karstryggen Formation, East Greenland

L. Stemmerik

doi:10.1007/bfb0011372

Cyclic carbonate and sulphate from the Upper Permian Karstryggen Formation, East Greenland

L. Stemmerik

Department of Geo-energy and Storage

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

5 Citations (Scopus)

Abstract

Four different types have been recognised. Type 1 and 2 cycles were formed as the result of repeated subaerial exposure of lagoonal sediments. Type 3 and 4 cycles were formed as shallow, high-energy shoal sediments became exposed. These cycles result from rapid fluctuations of sea-level. The fluctuations were too rapid to allow facies progradation of any significance and the different cycles aggrade and are therefore very localized. -from Author

Original language	English
Title of host publication	The Zechstein facies in Europe
Editors	T.M. Peryt
Publisher	Springer
Pages	5-22
Number of pages	18
Volume	Lecture notes in Earth Sciences 10
DOIs	https://doi.org/10.1007/bfb0011372
Publication status	Published - 1987

Programme Area

Programme Area 3: Energy Resources

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10.1007/bfb0011372

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title = "Cyclic carbonate and sulphate from the Upper Permian Karstryggen Formation, East Greenland",

abstract = "Four different types have been recognised. Type 1 and 2 cycles were formed as the result of repeated subaerial exposure of lagoonal sediments. Type 3 and 4 cycles were formed as shallow, high-energy shoal sediments became exposed. These cycles result from rapid fluctuations of sea-level. The fluctuations were too rapid to allow facies progradation of any significance and the different cycles aggrade and are therefore very localized. -from Author",

author = "L. Stemmerik",

year = "1987",

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volume = "Lecture notes in Earth Sciences 10",

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T1 - Cyclic carbonate and sulphate from the Upper Permian Karstryggen Formation, East Greenland

AU - Stemmerik, L.

PY - 1987

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N2 - Four different types have been recognised. Type 1 and 2 cycles were formed as the result of repeated subaerial exposure of lagoonal sediments. Type 3 and 4 cycles were formed as shallow, high-energy shoal sediments became exposed. These cycles result from rapid fluctuations of sea-level. The fluctuations were too rapid to allow facies progradation of any significance and the different cycles aggrade and are therefore very localized. -from Author

AB - Four different types have been recognised. Type 1 and 2 cycles were formed as the result of repeated subaerial exposure of lagoonal sediments. Type 3 and 4 cycles were formed as shallow, high-energy shoal sediments became exposed. These cycles result from rapid fluctuations of sea-level. The fluctuations were too rapid to allow facies progradation of any significance and the different cycles aggrade and are therefore very localized. -from Author

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U2 - 10.1007/bfb0011372

DO - 10.1007/bfb0011372

M3 - Chapter in book

AN - SCOPUS:0023584625

VL - Lecture notes in Earth Sciences 10

SP - 5

EP - 22

BT - The Zechstein facies in Europe

A2 - Peryt, T.M.

PB - Springer

ER -

Cyclic carbonate and sulphate from the Upper Permian Karstryggen Formation, East Greenland

Abstract

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