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- W813014716 abstract "Many inconspicious indications of thrusting were found at Renirie Rocks. The nunatak consists mainly of gra nitic rocks of Granite Harbour Intrusives. The southernmost end only is made up of agmatitic migmatites. Mar ked shearplanes with a slickenside-like appearance are rare in the migmatites and in the western and central gra nitoids but increase in abundance to the northeast, down the slope to the Rennick Glacier. Their spacing lies between 10 cm and I m, sometimes even closer. Most of these shearplanes form discrete surfaces, but towards the NE there are shearzones more than 5 cm wide and deformation zones with a collective width of 75 cm. The shear surfaces are often overprinted by glacial striations and therefore sometimes hard to distinguish." @default.
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- W813014716 date "1992-11-14" @default.
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- W813014716 title "15. The Southern Continuation of the Wilson Thrust" @default.
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