...E. Van der Flier-Keller; W. S. Fyfe Abstract Cretaceous coal-bearing sequences from the Moose River basin in northern Ontario and the Peace River basin in northeast British Columbia were analysed for trace- and major-element contents. Modes of occurrence of the trace elements are proposed...

... isotopes of the Peace River Arch in the Western Canada Sedimentary Basin: A framework for resolving deep basin lithium sources Cody N. Lazowski1 Boriana Kalderon-Asael2, Dan Asael2, Maria L. Arizaleta1, Scott Melnyk1, Sasha Wilson1, Daniel S. Alessi1, Noah J. Planavsky2, Kurt O. Konhauser1, and Murray K...

... Gagnon BULLETIN OF CANADIAN PETROLEUM GEOLOGY VOL. 47, NO. 4 (DECEMBER, 1999), E 594-620 Stratal reorientation, depositional processes, and sequence volution of the Cretaceous in the Peace River Arch region of the Western Canada Sedimentary Basin DONGQING CHEN Department of Geology University of Regina...

...D.R. Issler; C. Beaumont; S.D. Willett; R.A. Donelick; J. Mooers; A. Grist ABSTRACT Apatites separated from Cretaceous, Devonian and Precambrian petroleum exploration drill core samples from the Peace River Arch area of the Western Canada Sedimentary Basin have been analyzed for their fission-track...

... (Big Snowy Group)-Tyler contact. In Alberta (Peace River area) the Mississippian-Pennsylvanian boundary was found to be at the Golata-Kiskatinaw contact. The Golata formation is very likely correlative with part of the Big snowy Group; the Kiskatinaw formation is believed to be the age equivalent...

... of a foreland basin in western Canada. Triassic sedimentation in western Canada was centred on four basins or subbasins: the extensional or transtensional Peace River Basin, the transtensional Liard Basin, an unnamed continental margin sag basin, and the Williston Basin. This paper covers only the Peace River...

...Graham R. Davies; Thomas F. Moslow; Mike D. Sherwin ABSTRACT The Lower Triassic Montney Formation was deposited in a west-facing, arcuate extensional basin, designated the Peace River Basin, on the northwestern margin of the Supercontinent Pangea, centred at about 30°N paleolatitude. At least...

...G. R. Davies ABSTRACT The carbonate-dominant Upper Triassic Baldonnel and Pardonet formations were deposited in the west-facing extensional Peace River Basin, in a midlatitudinal setting on the northwestern margin of the supercontinent Pangea. Subsurface distribution of the Pardonet is restricted...

... are summarized and the sequence biostratigraphic framework provides a template demonstrating the correlation potential of the Montney Formation in the Peace River Basin from west-central Alberta to east-central British Columbia. The Montney Formation, which includes three 3rd order depositional sequences...

... into the Peace River Basin as a result of periodic reactivation of the Dawson Creek Graben Complex and subsequent sediment loading over the southern portion of the reservoir trend. Effective porosity is primarily intergranular in the reservoir sandstone facies, and significant moldic and intragranular porosity...

... into tilted blocks. Those grabens extending across the continental margin and normal to it, are aulacogens, opening into the geosyncline to the west. All these fractures are rejuvenated, Precambrian basement features. The Liard Plateau in northeastern British Columbia, the Peace River basin in northwestern...

... the nature and extent of the initial Carboniferous basins and how they relate to the underlying Peace River Arch. The Banff Formation is a shallowing-upward succession, from slope and basin carbonate and shale in the lower part, to shallow and restricted shelf and shoreline carbonate and sandstone at the top...

... the Lower Mississippian beds are preserved on the plains, although Upper Mississippian strata occur in the Peace River area and south of the International Boundary in the Williston basin area. The thickest sections of Lower and Upper Mississippian are found along the eastern ranges of the Rocky Mountains...

... component to the east and north, a thicker slope component and a thin basin deposit to the west. The units are arranged in a shingling fashion from east to west. This pattern was obstructed to the west by the stable Peace River Arch so that the upper units are incomplete, lacking the basin and in some cases...

... of structural and sedimentary features in the region. During its history, the Peace River Arch has existed in three different forms: a Late Proterozoic to early Paleozoic Arch, a late Paleozoic to earliest Mesozoic Embayment, and as a deep basin component of a Mesozoic foreland basin. During the late Middle...