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- W2276924503 abstract "ABSTRACT In the past, the contact between the Scollard and Paskapoo formations in central Alberta has been interpreted by some authors as regionally disconformable, and by others as conformable with local erosion. In this study, two sections are examined paleomagnetically for evidence of the magnitude of the disconformity. It is found that polarity zone 28 and half of 28r are missing from the Scollard Formation at Scollard Canyon, whereas all of 28r and most of 28 are present in the Ardley area some 50 km to the northwest. Therefore the sub-Paskapoo disconformity at Scollard Canyon represents a hiatus of approximately 1.25 m.y. RESUME Dans le passe, certains auteurs avaient interprete le contact entre les formations Scollard et Paskapoo comme etant discordant a l'echelle regionale, et d'autres l'avaient interprete comme etant conforme a l'erosion locale. Dans la presente etude, deux coupes sont examinees du point de vue paleomagnetique afin d'obtenir des preuves de l'ampleur de la discordance. Il est demontre que la zone de polarite 28 et la moitie de 28r sont manquantes dans la formation Scollard a Scollard Canyon, tandis la totalite de 28r et la plus grande partie de 28 y sont presentes dans la region de Ardley, situee a quelques 50 km en direction nord-ouest. Donc la discordance sous la formation Paskapoo a Scollard Canyon represente un hiatus de 1,25 Ma. Traduit par Marc Charest" @default.
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- W2276924503 date "1990-06-01" @default.
- W2276924503 modified "2023-09-27" @default.
- W2276924503 title "Magnetostratigraphic Evidence Bearing on the Magnitude of the Sub-Paskapoo Disconformity in the Scollard Canyon-Ardley Area of the Red Deer Valley, Alberta" @default.
- W2276924503 doi "https://doi.org/10.35767/gscpgbull.38.2.197" @default.
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