Topographic Evolution of the Sierra Nevada Measured Directly by Inversion of Low-temperature Thermochronology

Abstract

At present, there are at least two competing ideas for the topographic evolution of the Sierra Nevada. One idea is that the Sierra Nevada was formed as a monocline in the Cretaceous, marking the transition from the Great Valley forearc basin to the west, and a high Nevadaplano plateau to the east, similar to the west flank of the modern Altiplano of the… (More)

9 Figures and Tables

Topics

  • Presentations referencing similar topics