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W2121373721 abstract "The Laxford front is a candidate for a partial section across a major sub-vertical ductile shear belt which was active for more than 1000 Ma from at least 2800 Ma. Determinations of heterogeneous shear strain from major structural patterns indicate a minimum finite dextral displacement of 35 km. Three minimum strain estimates have been determined; finite strain from the end of the granulite facies metamorphism, strain from the late-Scourian and the Laxfordian strain. Most of the determined shear strain occurred in the Scourian; dextral displacements with movement directions plunging about 40° SE played a major part. The highest shear strains for each stage occurred over an early Scourian synform containing supracrustal rocks and the width of the shear belt increased throughout progressive deformation. The shear belt may be wedge-shape, narrowing westwards and downwards as the result of modification by superposed strain in the north and west of the structure. A model is proposed for both the spatial and temporal distribution of strain throughout this major shear belt which may be of use in the study of generalised shear belt evolution. It may be profitable to review the interpretations of other NW trending belts in the Precambrian basement of Britain in the light of this evidence." @default.
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W2121373721 date "1978-01-01" @default.
W2121373721 modified "2023-09-30" @default.
W2121373721 title "Progressive simple shear deformation on the Laxford Shear Zone, Sutherland" @default.
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W2121373721 doi "https://doi.org/10.1016/s0016-7878(78)80011-x" @default.
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