--> Abstract: A Tidally-Influenced, Seasonally Active Delta Front: the Lower Triassic Montney Formation, Kaybob and Kaybob South Hydrocarbon Fields Area, West-Central Alberta, Canada, by Demian J. C. Robbins and S. George Pemberton; #90914(2000)

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Demian J. C. Robbins1, S. George Pemberton1
(1) Ichnology Research Group, Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB

Abstract: A tidally-influenced, seasonally active delta front: the Lower Triassic Montney Formation, Kaybob and Kaybob South hydrocarbon fields area, west-central Alberta, Canada

The subsurface Montney Formation (Lower Triassic) of west-central Alberta, Canada, comprises a westward-dipping wedge of fine-grained siliciclastic sediments truncated in the east by later Mesozoic erosion. The eastern subcrop edge of the Montney is characterized by a mixed assemblage of palaeoshoreline-proximal siltstones, very fine sandstones and bioclastic coquinas of enigmatic origin.

In the vicinity of the Kaybob and Kaybob South hydrocarbon fields, both significant producing Montney reservoirs, the siliciclastic accumulations are dominated by an association of eight lithofacies grouped into two facies assemblages. Facies Assemblage I (FA1) predominates, and comprises three gradationally interbedded facies characterized by fine lamination, locally abundant pyrite, tidally-associated sedimentary structures and near-rhythmic but intermittent sedimentation. Facies Assemblage II (FA2) comprises five facies characterized by rapid deposition, soft-sediment deformation and dewatering, and occurs as isolated accumulations within FA1 successions.

Ichnofossils associated with FA1 comprise a locally abundant but low-diversity assemblage representative of an impoverished Skolithos ichnofacies. Lingulichnus is predominant. Additional forms include Teichichnus, Thalassinoides, Planolites, Palaeophycus, Skolithos, and Diplocraterion. Ichnofossil preservational styles and distributions define important environmental parameters not apparent from sedimentological observations. These include locally elevated sedimentation rates and significant ecological gradients such as salinity, oxygen and food supply variations.

FA1 deposits represent a seasonally active delta front normally sheltered from the open shelf. Sedimentation was subject to significant tidal influence and penecontemporaneous reworking. FA2 represents mixed allocyclic and autocyclic perturbations of the deltaic setting, including episodic storm deposits and meso- to macro-scale slumping events.

AAPG Search and Discovery Article #90914©2000 AAPG Annual Convention, New Orleans, Louisiana