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- W2118603290 abstract "Late Archean lamprophyre dikes crop out on both sides of the Quetico–Shebandowan subprovince boundary. They post date F 1 folds in late Archean rocks (2690 Ma) but their intrusion overlapped with the waning phase of S 1 development. S 1 developed to varying degrees or is absent in some dikes. Nevertheless, the dikes show a cryptic tectonic fabric in the ferromagnetic minerals revealed by anisotropy of magnetic susceptibility (AMS). This is parallel to S 1 in the host metamorphic rocks. Thus, the S 1 fabric-forming episode may be correlated from one subprovince to the other using the dike swarm as a chronological marker." @default.
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- W2118603290 date "1994-09-01" @default.
- W2118603290 modified "2023-10-15" @default.
- W2118603290 title "A magnetotectonic study correlating late Archean deformation in northwestern Ontario" @default.
- W2118603290 doi "https://doi.org/10.1139/e94-128" @default.
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