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Table 5 Relative contributions (and uncertainty expressed as the standard deviation) of the three end member sources in the catchment to the three in-stream locations Lan-1, Lan-5 and Lan-10 (see Fig. 2)

From: Differential erosion and sediment fluxes in the Landquart basin and possible relationships to lithology and tectonic controls

Model run In-stream location GOF Sedimentary contribution (%) Crystalline contribution (%) Ophiolitic contribution (%)
1 (all elements) Lan-1 80 73 ± 6 6 ± 7 22 ± 7
Lan-5 77 45 ± 6 6 ± 7 50 ± 7
Lan-10 72 42 ± 6 6 ± 7 51 ± 7
2 (Na2O, Ni, Sr, Sc) Lan-1 93 72 ± 7 21 ± 8 7 ± 7
Lan-5 91 37 ± 8 30 ± 12 32 ± 8
Lan-10 86 32 ± 10 42 ± 16 26 ± 11
  1. The quality of the model performance is given as goodness of fit (GOF)