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- W2030764077 abstract "Current research in SW Namibia recognises the Gariep arc as a southerly extension to the Damaran orogenic front of central and northern Namibia. We consider the Gariep arc to have evolved by large-scale thrusting of cover sediments and basement gneisses as flat-lying sheets emplaced to the south-east. Basic rocks with ophiolitic affinities are confined to the highest thrust sheet. However, due to the gravitational instability caused by virtue of its high density, this obducted mass collapsed onto a previously undeformed foreland centred in the Schakalsberg Mountains. Localised extensional flow beneath the thrust sheet initiated a series of imbricate thrust slices emplacing cover sediments and basement to the south-east onto a new foreland now located east of Rosh Pinah. A model of differential movement in a thrust regime, probably due to localised spreading of an obducted mass, is suggested for the origin of the observed arcuate structures." @default.
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- W2030764077 date "1982-04-01" @default.
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- W2030764077 title "The structural evolution of the Gariep arc in southern Namibia (South-West Africa)" @default.
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- W2030764077 doi "https://doi.org/10.1016/0301-9268(82)90023-7" @default.
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