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Table 2 Mineral assemblages and physical properties of inferred lithologies for sub-IBM crust and mantle

From: Evolution of the Earth as an andesite planet: water, plate tectonics, and delamination of anti-continent

Layer

Middle crust

Lower crust

Upper mantle

Composition

1:1 mixture

3:2 mixture

7:3 mixture

Basalt

Restite

Restite + 10 % olivine

Harzburgite

Depth (km)

5

8.5

11

5

9

11

5

10

11

11

12

20.5

25

25

27

40

25

30

40

40

50

70

T (°C)

300

380

430

300

390

430

300

410

430

430

450

650

750

750

780

970

750

820

970

970

1113

1400

Quartz

31.7

31.6

31.9

26.9

26.8

27.0

22.0

21.8

22.0

6.2

6.3

7.2

7.3

1.5

2.6

4.1

      

Plagioclase

34.8

34.8

33.6

36.8

37.0

35.9

38.8

38.8

38.1

45.3

44.5

34.4

32.2

36.6

32.2

26.0

20.4

17.1

17.1

   

Alkali feldspar

4.5

4.5

4.5

3.8

3.7

3.8

3.1

3.0

3.1

0.7

0.7

0.7

0.7

0.2

0.2

0.2

0.2

0.2

0.2

   

Hornblende

22.0

22.0

22.1

22.2

22.2

22.3

22.5

22.5

22.6

23.4

23.4

24.2

24.4

         

Garnet

 

0.4

2.3

 

0.2

1.9

 

0.4

1.4

 

1.4

19.3

20.5

27.1

32.1

33.5

34.6

36.8

37.0

   

Olivine

                   

80.0

80.0

80.0

Orthopyroxene

5.1

4.8

3.5

6.9

6.9

5.7

8.8

8.6

7.9

14.9

14.0

0.0

0.0

4.3

  

8.4

7.2

6.7

20.0

20.0

20.0

Clinopyroxene

1.3

1.3

1.4

2.6

2.6

2.7

4.1

4.1

4.2

8.7

8.9

13.3

14.4

29.8

32.3

35.6

35.6

37.7

38.5

   

Ilmenite

0.6

0.6

0.6

0.7

0.7

0.7

0.7

0.7

0.7

0.9

0.9

0.9

          

Rutile

            

0.5

0.6

0.6

0.6

 

0.5

0.5

   

ρ (g/cm3)

2.92

2.93

2.95

2.96

2.96

2.98

3.00

3.00

3.01

3.11

3.12

3.27

3.26

3.35

3.38

3.40

3.46

3.46

3.46

3.25

3.24

3.20

V P (km/s)

6.50

6.51

6.54

6.57

6.56

6.59

6.63

6.63

6.65

6.82

6.85

7.13

7.14

7.33

7.45

7.48

7.60

7.64

7.62

7.86

7.81

7.51

V S (km/s)

3.82

3.81

3.82

3.82

3.80

3.82

3.82

3.80

3.81

3.80

3.82

3.98

3.99

4.06

4.12

4.14

4.23

4.25

4.23

4.49

4.44

4.22

Poisson’s ratio

0.24

0.24

0.24

0.24

0.25

0.25

0.25

0.25

0.25

0.27

0.27

0.27

0.27

0.28

0.28

0.28

0.27

0.28

0.28

0.26

0.26

0.27