Pleistocene uplift, climate and morphological segmentation of the Northern Chile coasts (24°S-32°S): Insights from cosmogenic 10Be dating of paleoshorelines
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文摘

We date paleoshorelines in Chile between 24°S and 32°S using 10Be concentrations data.

Post-emergence erosion of abrasion shore terraces approaches 1 m/Myr.

The coast has been uplifting at ~ 0.3 mm/yr during the Upper Pleistocene.

Uplift velocity increased during the Pleistocene following a period of stability.

Paleoshorelines are poorly preserved beneath the northern coastal scarp.

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