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Figure 7 | Progress in Earth and Planetary Science

Figure 7

From: Direct comparison of site-specific and basin-scale denudation rate estimation by in situ cosmogenic nuclides: an example from the Abukuma Mountains, Japan

Figure 7

Plot of 26 Al/10 Be ratios versus 10 Be concentration of fluvial samples with 1 σ errors. 10Be concentrations are normalized for values at sea level and high latitude. Zero denudation and steady-state denudation lines are shown as solid lines. 26Al/10Be ratios indicate that these samples do not have complex exposure histories detected by the 26Al/10Be system.

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