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- W1652376870 abstract "The relationship between flood basalts and feeder dikes is investigated through an anisotropy of magnetic susceptibility (AMS) study of the 200 Ma Central Atlantic Magmatic Province (CAMP) in the Fundy basin of southeastern Canada. Over a 200 km strike length the North Mountain basalts exhibit a consistent N-NE (or S-SW) emplacement direction flow pattern (based on the orientation of maximum AMS axes). Less definitively, the data suggest that the lower lavas (including the Grand Manaan basalts) have a NE-SW flow axis, while the middle and upper flow units have a more N-S flow axis. The Swallowtail dike of Grand Manaan Island exhibits sub-vertical flow based on AMS data. Its presumed extension along the axial zone of the Fundy basin is the possible feeder for at least the middle and upper North Mountain flows." @default.
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- W1652376870 date "2003-01-01" @default.
- W1652376870 modified "2023-09-27" @default.
- W1652376870 title "Magma flow pattern in the North Mountain basalts of the 200 Ma CAMP event: Evidence from the magnetic fabric" @default.
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- W1652376870 doi "https://doi.org/10.1029/136gm12" @default.
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