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- W2023182024 abstract "Mesozoic sedimentation in northern East Greenland was initiated in the Middle Jurassic with transgression of the peneplaned Caledonian basement. Approximately 1 km of inshore and shelf sediments were deposited in progressively deeper water in Middle and Late Jurassic times. The sedimentary sequence is interpreted as resulting from the interplay of fault-controlled subsidence, borderland uplift, and major eustatic sea-level changes. Facies analysis shows that sedimentation in the rift-type basin was influenced by fluvial, tidal, wave, and storm-related processes." @default.
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- W2023182024 date "1983-03-01" @default.
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- W2023182024 title "Rift propagation and eustacy as controlling factors during jurassic inshore and shelf sedimentation in Northern East Greenland" @default.
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- W2023182024 doi "https://doi.org/10.1016/0037-0738(83)90083-0" @default.
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