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- W2095502627 abstract "The Rottenstone and western La Ronge domains of the south—central Churchill province in Saskatchewan consist mostly of Hudsonian batholithic complexes spatially and structurally related to an Aphebian—Hudsonian volcanic arc. The batholithic belt is of comparable dimensions and compositional variation to Cordilleran-type Phanerozoic batholiths and appears to be emplaced in close proximity to a prior late Archean—early Aphebian continental crustal margin. A “quartz-diorite line” separating dominant quartz-diorite—tonalite—granodiorite plutonic rocks from dominant granodiorite—quartz-monzonite—granite intrusives can be defined. These general characteristics, as well as more detailed features of Aphebian deposition and Hudsonian thermotectonism within and on either side of the Rottenstone domain, suggest a continental margin, rather than an “intracontinental” location, for evolution of the Hudsonian orogenic belt of the south—central Churchill province and provide some insights into the possible development of this part of the Canadian shield as part of a Hudsonian Wilson Cycle." @default.
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- W2095502627 date "1981-06-01" @default.
- W2095502627 modified "2023-09-27" @default.
- W2095502627 title "A cordilleran-type batholitic belt in the Churchill province in northern Saskatchewan" @default.
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- W2095502627 doi "https://doi.org/10.1016/0301-9268(81)90042-5" @default.
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