Anatomy of ancient passive margin slope systems: Aptian gravity-driven deposition on the Vocontian palaeomargin, western Alps, south-east France

The Aptian succession on the Vocontian palaeomargin (south‐east France) consists of marl and marly calcareous pelagic slope facies together with a range of gravity‐driven deposits (slumps, debris‐flow deposits, turbidite packages and massive sandstones). The massive sandstones were emplaced by high‐...

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Veröffentlicht in:	Sedimentology 2003-12, Vol.50 (6), p.1231-1270
Hauptverfasser:	Friès, Gérard, Parize, Olivier
Format:	Artikel
Sprache:	eng
Schlagworte:	Aptian basin analysis gravity-driven deposits sequence stratigraphy slope turbidites
Online-Zugang:	Volltext
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