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- W2154756908 abstract "ABSTRACT The Upper Devonian to Lower Mississippian Bakken Formation, Williston Basin, consists of: 1) a black mudstone Lower member; 2) a gray mudstone and sandstone Middle member; and 3) a black mudstone Upper Member. Nine lithofacies are recognized; a black mudstone that characterizes the Lower and Upper members and eight remaining gray mudstone and sandstone lithofacies from the Middle member. The hemipelagic black mudstone of the Lower and Upper members accumulated in a distal deep water ( 200 m), dans des conditions de fond stagnantes qui sont caracterisees par: 1) des eaux de fond tranquilles remuees peridiquement par des courants de fond lents; 2) un faible taux de sedimentation clastique; et 3) un substratum prive de microfaune benthique a cause de l'etat anoxique des eaux de fond contenant des concentrations elevees et probablement toxiques d'hydrogene sulfure en solution. Les schistes argileux et les gres du Membre moyen de la formation Bakken s'accumulere dans un milieu marin en eau peu profonde au large des cotes (10-200 m), et dans un environnement de zone infratidale inferieure, moyenne et superieure (< 10 m). Les empreintes fossiles dans le Membre moyen suggerent un ichnofacies de Nereites et Cruziana changeant graduellement en ichnofacies de Skolithos, ce qui soutient l'interpretation d'un ancien milieu marin d'eau peu profonde. Le depot de trois membres distincts de la formation Bakken reflete des changements importants dans la profondeur de l'eau dans le Bassin de Williston, qui resulte des changements relatifs dans le niveau marin. Traduit par Marc Charest." @default.
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- W2154756908 date "1996-09-01" @default.
- W2154756908 modified "2023-09-23" @default.
- W2154756908 title "Lithofacies and paleoenvironments of the Upper Devonian and Lower Mississippian Bakken Formation, Williston Basin" @default.
- W2154756908 doi "https://doi.org/10.35767/gscpgbull.44.3.495" @default.
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