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- W2016459170 abstract "The Shuswap terrane, exhibiting flow cleavage parallel to the sedimentary stratification over a wide area, has been regarded as a classic example of load or static metamor-phism. An examination of the structure of the gneisses reveals a common quaquaversal habit due to the updoming of granite stocks into the flat-lying, deeply buried sediments. The effect of the upward thrust of the magma against a great load differs from the effect of load alone. In the latter case the pressure would be hydrostatic and the deformation resulting would be merely dilatational, and consequently without orientation of the constituent minerals. In the former case, however, the shouldering effect of the magma results in the compression of the strata normal to the bedding, and a complementary elongation of the strata in their long dimension, supplying the lateral relief necessary to cause an orientation of the minerals. This explanation applies both to the gneisses (Shuswap) and to the overlying schists (Beltian). The yielding of the intruded rocks by rock flowage, the result of an active thrust of the subjacent magma, clearly cannot be regarded as static." @default.
- W2016459170 created "2016-06-24" @default.
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- W2016459170 date "1934-10-01" @default.
- W2016459170 modified "2023-10-14" @default.
- W2016459170 title "The Metamorphism of the Shuswap Terrane of British Columbia" @default.
- W2016459170 doi "https://doi.org/10.1086/624235" @default.
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