4.3 Article

Cenozoic slip along the southern Sierra Nevada normal fault, California (USA): A long-lived stable western boundary of the Basin and Range

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Summary: The tectonic interpretation of the central Sierra Nevada remains controversial, with a study providing evidence for late Cenozoic uplift of the mountain range. By examining the Trachyandesite of Kennedy Table, researchers concluded that the uplift was not a result of continuous tilting, but a distinct event in the late Cenozoic. Using quantitative data, it was estimated that the uplift of the Sierran block was around 2,000 to 3,000 meters, confirming earlier assumptions.

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