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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)