Spacing and strength of active continental strike-slip faults
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Parallel and evenly spaced active strike-slip faults occur widely in nature.

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Stress-shadow model quantifies spacing as function of strength and stress state.

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Analogue experiments confirm model assumptions and test predictions.

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Fault spacing and seismogenic zone thickness used to estimate absolute fault friction.

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Active strike-slip faults in Asia are weaker than those along the San Andreas.

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