Jf. Lerbekmo et Ar. Sweet, Magnetostratigraphy and biostratigraphy of the continental Paleocene in the Calgary area, southwestern Alberta, B CAN PETRO, 48(4), 2000, pp. 285-306
A chronology for Paleocene strata of the Calgary region is developed from t
he integration of magnetostratigraphy with palynological and mammal zones.
Structural reference to the underlying Battle Formation adds stratigraphic
control. These strata range in age from magnetochron 29r to the lower half
of 26r and palynomorph zones Wodehouseia fimbriata through Aquilapollenites
spinulosus. Four mammal sites have been placed in the magnetostratigraphic
framework. The youngest is a Tiffanian (Ti1) site in 26r. Sites judged to
be Torrejonian occur in 27n, 28r and 29n. The presence of thin coals indica
tes correlation of lower Paleocene outcrops south and southeast of Calgary
to the upper Scollard Formation. Younger strata in Calgary City have charac
teristics of a seasonally dry facies association most comparable to that of
the Porcupine Hills Formation of southwestern Alberta. To the west and nor
th of Calgary, the occurrence of thin coals in strata of late Paleocene age
justifies assigning these rocks to the Paskapoo Formation. However, the pl
acement of all formational boundaries is somewhat arbitrary in this transit
ional region between the nomenclatural systems of southwestern versus centr
al Alberta. The type Porcupine Hills Formation is shown to be correlative t
o the upper part of the upper Scollard Formation and the lower part of the
Paskapoo Formation.