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- W2051276102 abstract "Six BIRPS deep Seismic reflection profiles around the British Isles that cross the trend of the lapetus suture allow a geophysical definition of the suture zone for 900 km along its strike and demonstrate that specific reflective structures have survived since the mid-Palaeozoic Caledonian orogen. In an area northeast of England, spanning 70 km along Caledonian strike and 200 km across strike, three profiles show very considerable similarities in the reflectivity patterns of the lower crust. When these similarities are mapped, the boundaries separating regions of lower crust with the same reflective character run parallel to Caledonian strike. This strongly suggests that the distribution of reflectivity in the lower crust in this area is directly controlled by Caledonian structures. Geologic models for the area imply that many of the reflectors themselves may also be of Caledonian age. However, though an age for the imposition of patterns of reflectivity can be inferred, the age of an individual reflector cannot be determined unless it can be traced to outcrop or unless there is independent evidence as to the physical nature of the reflector." @default.
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- W2051276102 date "1990-02-01" @default.
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- W2051276102 title "Dating the source of lower crystal reflectivity using BIRPS deep Seismic profiles across the lapetus suture" @default.
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- W2051276102 doi "https://doi.org/10.1016/0040-1951(90)90237-3" @default.
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