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- W2023896004 abstract "Structural and geomorphic analysis of late Holocene sediments in the Lake County region of the New Madrid seismic zone indicates that they are deformed by fault-related folding above the blind Reelfoot thrust fault. The widths of narrow kink bands exposed in trenches were used to model the Reelfoot scarp as a forelimb on a fault-bend fold; this, coupled with the age of folded sediment, yields a slip rate on the blind thrust of 6.1 +/- 0.7 mm/year for the past 2300 +/- 100 years. An alternative method used structural relief across the scarp and the estimated dip of the underlying blind thrust to calculate a slip rate of 4.8 +/- 0.2 mm/year. Geometric relations suggest that the right lateral slip rate on the New Madrid seismic zone is 1.8 to 2.0 mm/year." @default.
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- W2023896004 date "1999-11-05" @default.
- W2023896004 modified "2023-10-14" @default.
- W2023896004 title "Fault Slip Rates in the Modern New Madrid Seismic Zone" @default.
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- W2023896004 doi "https://doi.org/10.1126/science.286.5442.1135" @default.
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