Stress development in heterogenetic lithosphere: Insights into earthquake processes in the New Madrid Seismic Zone
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文摘

Numerical models test the effects of lithospheric heterogeneities on earthquakes.

A mantle low-velocity zone facilitates lithospheric stress localization.

High differential stresses reactivate fossil faults and trigger earthquakes.

A strong lower crust in NMSZ prevents decoupling of the mantle and upper crust.

In the Midcontinent “normal” mantle does not catalyze stress development.

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