@inbook{9f417d8860c848769e87959182d8c328,
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 = "Lars Stemmerik",
year = "1987",
doi = "10.1007/bfb0011372",
language = "English",
isbn = "978-3-540-17710-4",
series = "Lecture notes in Earth Sciences",
publisher = "Springer",
pages = "5--22",
editor = "Peryt, {Tadeusz M.}",
booktitle = "The Zechstein facies in Europe",
address = "China",
}