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The development of clast fabric in mudflows
Journal of Sedimentary Research (1968) 38 (4): 1242–1253.
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Field evidence suggests that the Palaeoproterozoic Gowganda Formation in Canada is non-glacial in origin
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Fabric, paleomagnetism, and interpretation of pre-illinoian diamictons and paleosols on Cloudy Ridge and Milk River Ridge, Alberta and Montana
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- Rene W. Barendregt
Géographie physique et Quaternaire (2004) 55 (2): 141.