Hybrid event beds dominated by transitional‐flow facies: character, distribution and significance in the Maastrichtian Springar Formation, north‐west Vøring Basin, Norwegian Sea

Hybrid event beds comprising clay‐poor and clay‐rich sandstone are abundant in Maastrichtian‐aged sandstones of the Springar Formation in the north‐west Vøring Basin, Norwegian Sea. This study focuses on an interval, informally referred to as the Lower Sandstone, which has been penetrated in five we...

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Veröffentlicht in:	Sedimentology 2017-04, Vol.64 (3), p.747-776
Hauptverfasser:	Southern, Sarah J., Kane, Ian A., Warchoł, Michał J., Porten, Kristin W., McCaffrey, William D., Talling, Peter
Format:	Artikel
Sprache:	eng
Schlagworte:	Clay‐rich sandstone hybrid event bed hybrid flow transitional flow turbidite
Online-Zugang:	Volltext
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