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Spacing and strength of active continental strike-slip faults
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文摘

Parallel and evenly spaced active strike-slip faults occur widely in nature.

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

Analogue experiments confirm model assumptions and test predictions.

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

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

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