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Table 5 As Table 4 but now for case 2 with stress- and temperature-dependent viscosity. In this case, \(z_\text {io}\) = 154

From: An introductory review of the thermal structure of subduction zones: II—numerical approach and validation

\(\varvec{f_m}\)

\(\varvec{T}_{\mathbf{ndof}}\)

\(\varvec{T}_{\mathbf{(200,-100)}}^*\)

(\(^\circ\)C)

\({\overline{{\varvec{T}}}}_{\varvec{s}}^*\)

(\(^\circ\)C)

\({\overline{{\varvec{T}}}}_{\varvec{w}}^*\)

(\(^\circ\)C)

\({\varvec{V}}_{{\mathbf{rms}},{\varvec{w}}}^*\)

(mm/yr)

TerraFERMA TH P2P1P2

2.0

21403

683.05

571.58

936.65

40.89

1.0

83935

682.87

572.23

936.11

40.78

0.5

332307

682.80

572.05

937.37

40.77

Sepran TH P2P1P2

     

2.0

17581

681.28

570.26

935.47

41.05

1.5

30947

682.48

570.73

937.11

40.91

1.0

68713

683.07

571.23

940.47

40.92

0.75

121574

682.97

571.62

941.23

41.00

0.5

270668

682.92

572.04

941.28

41.06

Sepran PF P2P2

     

2.0

17585

682.38

567.96

936.52

40.67

1.5

30851

683.67

569.60

942.73

40.63

1.0

68633

683.61

571.86

941.18

40.87

0.75

121366

683.03

571.77

940.32

40.98

0.5

270348

682.38

571.44

939.73

41.06