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- W2022706872 abstract "The westernmost part of the Proterozoic Grenville orogen, widely interpreted as an aggregate of structural domains and subdomains, has been subjected to superimposed disharmonic buckling on the scale of kilometres. The domain boundaries are characterized by abutments of upright to overturned folds attributed by others to thrust-induced truncation of inherited structures. The present study shows that abutments on geological maps are fold-termination lines which mark narrow zones of adjustment flow caused by buckle strain heterogeneity on the kilometre scale. Such adjustment zones are ductile equivalents of fold décollement surfaces in the brittle upper crust, and are normally characterized by high strain gradients. Prominent adjustment zones may be located within strain-softened rocks at domain boundaries coincident with major ductile thrusts." @default.
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- W2022706872 date "1991-01-01" @default.
- W2022706872 modified "2023-09-25" @default.
- W2022706872 title "The origin of fold abutments in the map pattern of the westernmost Grenville Province, central Ontario" @default.
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- W2022706872 doi "https://doi.org/10.1016/0301-9268(91)90055-f" @default.
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