Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology

Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology

Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology, Published online: 04 July 2018; doi:10.1038/s41586-018-0260-6

Reported acceleration of erosion in mountainous landscapes during the late Cenozoic is the result of combining thermochronology data with disparate exhumation histories, thereby converting spatial variations in erosion rates into temporal increases.

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