Experiment |
Vin (mm/yr) |
Thickness of
continental plate (km) |
Density
of Continental lithospheric mantle (kg/m3) |
Ocean-continent transition angle
(°) |
Depth of slab reach at 10
myr/ Time of subducted slab reach to 260 km |
Depth of slab reach at 10
myr/ Time of subducted slab reach to 260 km |
Crustal thickness of
overriding plate (km) |
Heat flow
(mW/m2) |
1 |
0 |
60 |
3275 |
15 |
15 |
230 km |
|
|
2 |
0 |
60 |
3275 |
30 |
30 |
5.5 myr |
22.9 |
94.8 |
3 |
0 |
60 |
3275 |
45 |
45 |
6.5 myr |
22.2 |
95.8 |
4 |
0 |
60 |
3275 |
60 |
60 |
no |
|
|
5 |
0 |
65 |
3275 |
15 |
15 |
no |
|
|
6 |
0 |
65 |
3275 |
30 |
30 |
8.7 myr |
22.9 |
80.6 |
7 |
0 |
65 |
3275 |
45 |
45 |
198 km |
|
|
8 |
0 |
65 |
3275 |
60 |
60 |
no |
|
|
9 |
0 |
70 |
3275 |
15 |
15 |
no |
|
|
10 |
0 |
70 |
3275 |
30 |
30 |
no |
|
|
11 |
0 |
70 |
3275 |
45 |
45 |
no |
|
|
12 |
0 |
70 |
3275 |
60 |
60 |
no |
|
|
13 |
0 |
60 |
3250 |
15 |
15 |
8.2 myr |
26.1 |
77.2 |
14 |
0 |
60 |
3250 |
30 |
30 |
4.5 myr |
23.2 |
97.8 |
15 |
0 |
60 |
3250 |
45 |
45 |
5.3 myr |
22.3 |
99.3 |
16 |
0 |
60 |
3250 |
60 |
60 |
192 km |
|
|
17 |
0 |
65 |
3250 |
15 |
15 |
no |
|
|
18 |
0 |
65 |
3250 |
30 |
30 |
7.1 myr |
22.8 |
82.9 |
19 |
0 |
65 |
3250 |
45 |
45 |
8.5 myr |
22.2 |
87.9 |
20 |
0 |
65 |
3250 |
60 |
60 |
no |
|
|
21 |
0 |
70 |
3250 |
15 |
15 |
no |
|
|
22 |
0 |
70 |
3250 |
30 |
30 |
190 km |
|
|
23 |
0 |
70 |
3250 |
45 |
45 |
no |
|
|
24 |
0 |
70 |
3250 |
60 |
60 |
no |
|
|
25 |
40 |
70 |
3275 |
30 |
30 |
4.6 myr |
28.2 |
79.5 |
26 |
40 |
75 |
3275 |
30 |
30 |
5.2 myr |
28.2 |
71 |
27 |
40 |
80 |
3275 |
30 |
30 |
5.6 myr |
28.9 |
65 |
28 |
20 |
70 |
3275 |
30 |
30 |
6.6 myr |
26.8 |
78.4 |
29 |
20 |
75 |
3275 |
30 |
30 |
8.3 myr |
27.7 |
70.5 |
30 |
20 |
80 |
3275 |
30 |
30 |
9.2 myr |
28.1 |
65.8 |
|
|
|
|
|
|
|
Model depth (km) |
Model depth (km) |
31 |
20 |
75 |
3275 |
30 |
30 |
6.1 myr |
670 |
670 |
32 |
20 |
75 |
3275 |
30 |
30 |
7.3 myr |
410 |
410 |
33 |
20 |
75 |
3275 |
30 |
30 |
9.3 myr |
360 |
360 |
34 |
20 |
75 |
3275 |
30 |
30 |
no |
310 |
310 |
35 |
20 |
75 |
3275 |
30 |
30 |
no |
260 |
260 |
36 |
20 |
75 |
3275 |
30 |
30 |
no |
210 |
210 |