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- W2024402610 abstract "Examples of Archean shield areas from Canada and Australia are used to demonstrate a consistent orthogonality in trend between late Archean mafic dikes (~2.5 Ga old) and the structure of granite–greenstone terrains whose orogenic history terminated no more than about 0.2 Ga prior to dike injection. The simplest explanation of this relationship is that the regional structural grain of the granite–greenstone terrains was formed by horizontal crustal compression, and that the direction of maximum horizontal stress remained unchanged up to and including the time of dike emplacement." @default.
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- W2024402610 date "1978-10-01" @default.
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- W2024402610 title "The structural relationship between Archean granite–greenstone terrains and late Archean mafic dikes" @default.
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- W2024402610 doi "https://doi.org/10.1139/e78-171" @default.
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