Pavy Formation

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Pavy Formation
Stratigraphic range: Thanetian
TypeFormation
Lithology
PrimarySiltstone
OtherCoal
Location
Coordinates81°42′N 64°24′W / 81.7°N 64.4°W / 81.7; -64.4Coordinates: 81°42′N 64°24′W / 81.7°N 64.4°W / 81.7; -64.4
Approximate paleocoordinates74°18′N 13°18′W / 74.3°N 13.3°W / 74.3; -13.3
RegionEllesmere Island, Nunavut
Country Canada
Extent
Type section
Named for
Pavy Formation is located in Canada
Pavy Formation
Pavy Formation (Canada)

The Pavy Formation is a geologic formation in Nunavut. It preserves fossil insects of ,[1] dating back to the Thanetian stage of the Paleocene period.

Description[]

The Pavy Formation is interpreted to be fluvial in origin. Trough-crossbedded sandstone facies dominate this formation and were probably channel deposits of a braided river system, with interbeds of siltstone and mudrock representing floodplain deposits. Where thicker intervals of mudrock occur, backswamp ponds or shallow-lake conditions were probably present. Only at Watercourse Valley and Pavy River did conditions stabilize long enough for swamps to develop, producing thick coal beds.

See also[]

References[]

  1. ^ Heer, 1878

Bibliography[]

  • Heer, O. 1878. Die Miocene Flora des Grinnell-Landes gegründet auf die von Capitan H.E. Feilden und Dr. E. Moss in der Nähe des Kap Murchison gesammelten fossilen Pflanzen. : Die Fossile Flora der Polarländer 5. 1-38.
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