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Spatio-temporal trends in normal-fault segmentation recorded by low-temperature thermochronology: Livingstone fault scarp, Malawi Rift, East African Rift System
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文摘

AHe thermochronology records normal fault segmentation on the Livingstone scarp.

Young AHe ages occur in the centre and old ages at the tip of fault segments.

Fault segmentation is only preserved because linkage occurred recently (<2 Ma).

Cenozoic Rifting commenced ca. 23 Ma, earlier than previously thought.

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