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- W2080772088 abstract "The foreland of Breidamerkurjökull, Iceland, is the only locality where tills known to have undergone subglacial deformation are exposed. Till on the foreland has a two-tiered structure, consisting of a dilatant upper horizon c 0.5 m thick and a compact lower till; these horizons correspond to the ductile deforming A horizon and the brittle-ductile B horizon observed below the glacier by G. S. Boulton and co-workers. The relationship between known strain history and a variety of macrofabric elements is examined for these two genetic facies of deformation till. The upper horizon exhibits variable a-axis fabrics and abundant evidence for clast re-alignment, reflecting ductile flow and rapid clast response to transient strains. In contrast, the lower horizon has consistently well organized a-axis fabrics with a narrow range of dip values, recording clast rotation into parallel with strain axes during brittle or brittle-ductile shear. The data indicate that till strain history imparts identifiable macrofabric signatures, providing important analogues to guide the interpretation of Pleistocene tills." @default.
- W2080772088 created "2016-06-24" @default.
- W2080772088 creator A5028501880 @default.
- W2080772088 date "1995-10-01" @default.
- W2080772088 modified "2023-10-18" @default.
- W2080772088 title "Fabric signature of subglacial till deformation, Breidamerkurjokull, Iceland" @default.
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- W2080772088 doi "https://doi.org/10.1111/j.1365-3091.1995.tb00406.x" @default.
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