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• W2041933460 endingPage "280" @default.
• W2041933460 startingPage "273" @default.
• W2041933460 abstract "U–Pb baddeleyite and zircon ages for three diabase dykes from widely spaced localities within the Grenville dyke swarm indicate a single age of emplacement at [Formula: see text] Ma. The 700 km long Grenville dyke swarm, located in the southeastern part of the Canadian Shield, was emplaced syntectonically with the development of the Ottawa graben. This graben may represent a plume-generated lapetan failed arm that developed at the onset of the breakup of Laurentia. Other precisely dated lapetan rift-related units, such as the Callander Alkaline Complex and the Tibbit Hill Formation volcanic rocks, indicate a protracted 36 Ma period of rifting and magmatism prior to volcanism along this segment of the lapetan margin. The age of the Grenville dykes is the youngest in a progression of precisely dated mafic magmatic events from the 723 Ma Franklin dykes and sills to the 615 Ma Long Range dykes, along the northern and northeastern margins of Laurentia, respectively. Thus, the age for these dykes represents a key time marker for continental breakup that preceded the formation of the Iapetus ocean." @default.
• W2041933460 created "2016-06-24" @default.
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• W2041933460 date "1995-03-01" @default.
• W2041933460 modified "2023-10-14" @default.
• W2041933460 title "Age of the Grenville dyke swarm, Ontario–Quebec: implications for the timing of lapetan rifting" @default.
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• W2041933460 doi "https://doi.org/10.1139/e95-022" @default.
• W2041933460 hasPublicationYear "1995" @default.
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