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Table 3 Proportions of potential sources contributing at successive ages

From: Provenance differentiation and earth surface process of the Mu Us sandy land constrained by detrital zircon U–Pb dating

Sample ID

SW MU (%)

NE MU (%)

West-Middle Hobq (%)

East Hobq (%)

Chinese Loess Plateau (%)

NE Tibetan Plateau

51

1

13

8

69

NE deserts

9

2

32

2

10

Northern Gobi

10

2

18

2

14

Tarim Basin

3

1

2

3

2

Western North China Craton

27

94

35

85

6