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

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Abstrakt

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

OriginalsprogEngelsk
TitelThe Zechstein facies in Europe
RedaktørerT.M. Peryt
ForlagSpringer
Sider5-22
Antal sider18
Vol/bindLecture notes in Earth Sciences 10
DOI
StatusUdgivet - 1987

Programområde

  • Programområde 3: Energiressourcer

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