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• W2045249543 startingPage "106" @default.
• W2045249543 abstract "Archean metasedimentary rocks in the eastern Point Lake area of the Slave Structural Province preserve a sequence of Archean structures consisting of two generations of folds (F 1 and F 2 ) with little associated penetrative cleavage and two subsequent generations of cleavage (S 3 and S 4 ) with little associated folding. Gneissic layering in the high-grade margin of the belt is composed of transposed bedding and the S 3 cleavage. Folding occurred prior to the thermal peak of metamorphism, whereas the develoment of subsequent cleavages spanned the thermal peak. The regional orientation of the folds and cleavages appears to be independent of the emplacement of granitoid intrusions, although their orientation is modified adjacent to syn- to late tectonic plutons. The supracrustal belt is interpreted as being part of a pre- to early metamorphic, west-verging fold (thrust?) belt whose strain pattern has been modified by post-folding, synmetamorphic shortening, and syn- to post-tectonic plutons. This deformation sequence is similar to those described in other supracrustal belts of the Slave Province and supports the concept that the Slave Province has undergone regional, horizontally directed compression before and during intrusion of large amounts of granitoids." @default.
• W2045249543 created "2016-06-24" @default.
• W2045249543 creator A5013178902 @default.
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• W2045249543 date "1989-01-01" @default.
• W2045249543 modified "2023-09-26" @default.
• W2045249543 title "Deformational history of an Archean fold belt, eastern Point Lake area, Slave Structural Province, N.W.T." @default.
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• W2045249543 doi "https://doi.org/10.1139/e89-009" @default.
• W2045249543 hasPublicationYear "1989" @default.
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