Extended Data Table 2 Composition and calculated density and viscosity of the North China lavas, MORB and Hawaii OIB

From: Widespread two-layered melt structure in the asthenosphere

Silicate melt

High Y/Yb lava

Low Y/Yb lava

Laoheishan

Hawaii OIB106

MORB45

Mean

1 SD

Mean

1 SD

basalt#

SiO2 (wt%)

41.76

1.45

46.91

1.72

39.93

47.92

50.49

TiO2 (wt%)

2.68

0.21

2.18

0.32

2.85

2.45

1.42

Al2O3 (wt%)

11.81

0.91

13.99

0.68

11.57

13.15

15.48

Fe2O3 (wt%)

15.03

0.77

12.43

0.78

16.57

12.50

10.39

MnO (wt%)

0.20

0.02

0.16

0.01

0.22

0.18

0.17

MgO (wt%)

10.09

1.66

9.81

1.32

9.85

9.89

7.84

CaO (wt%)

10.59

1.22

9.27

0.71

12.25

11.21

11.52

Na2O (wt%)

4.54

0.69

3.05

0.60

3.63

2.16

2.71

K2O (wt%)

2.18

0.40

1.63

0.34

2.04

0.31

0.18

P2O5 (wt%)

1.13

0.19

0.56

0.15

1.09

0.24

0.13

Na2O + K2O (wt%)

6.72

0.84

4.68

0.63

5.67

2.47

2.89

Fe/Mn ratio

68.3

6.0

69.2

4.9

68.0

61.8

54.9

Y/Yb ratio

20.81

1.40

14.36

0.98

21.87

13.51

10

Melt extraction depth (km)

149

11

98

8

158

91

63

Melt density (g/cm3)

3.291

 

3.096

 

3.351

3.086

2.942

Melt viscosity [log η (Pa s)]

0.988

 

1.412

 

0.851

1.460

1.730

Solid mantle density (g/cm3)

3.328

 

3.280

 

3.334

3.273

3.246

Melt mobility (Δρ/η)

0.085

 

0.130

 

−0.02

0.128

0.175

  1. Note: #Laoheishan basalt (15LHS05) is one extremely iron-rich and silica-poor sample from this study (Supplementary Table 2). The melt viscosity and density (Fe3+/∑Fe = 0.2; temperature was fixed at 1200 °C) were calculated using the method of ref. 72 and ref. 73, respectively. The depth of melt extraction was calculated according to the Y/Yb ratio, and then used to calculate the melt density and mobility (Δρ/η). Δρ is density contrast between solid mantle (Fo90 olivine as representative)98 and melt, and η is melt viscosity.