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• W2069630341 abstract "Many volcanoes emerge from the flank (footwall) of normal faults in continental rift zones. Because such locations are commonly topographically high and exhibit minor compressional structures, the association is enigmatic. A simple flexing plate model shows that deformation of a flexurally supported upper crust during normal faulting generates a dilational strain field in the footwall at the base of the crust. This strain field allows cracking and tapping of preexisting melt." @default.
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• W2069630341 date "1991-11-08" @default.
• W2069630341 modified "2023-09-30" @default.
• W2069630341 title "Structural Control of Flank Volcanism in Continental Rifts" @default.
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• W2069630341 doi "https://doi.org/10.1126/science.254.5033.839" @default.
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