Table 3 Flow law parameters
From: Sensitivity of elastic thickness to water in the Martian lithosphere
Rock type | Creep mechanism | A (s−1 MPa-n μmm) | n | m | σp (MPa) | E (kJ/mol) | V (cm3/mol) |
|---|---|---|---|---|---|---|---|
Plagioclase (wet) | Diffusion creepa | 101.7 | 1 | 3 | – | 170 | – |
Dislocation creepb | 10−5.6 | 4 | – | – | 235 | – | |
Peierls creepc | 10−1.2 | 2 | – | 3410 | 235 | – | |
Plagioclase (dry) | Diffusion creepa | 1012.1 | 1 | 3 | – | 467 | – |
Dislocation creepb | 100.9 | 3.9 | – | – | 431 | – | |
Peierls creepc | 103.5 | 2 | – | 9830 | 431 | – | |
Olivine (wet) | Diffusion creepd | 109.0 | 1 | 3 | – | 335 | 5 |
Dislocation creepe | 104.2 | 3 | – | – | 410 | 14 | |
Peierls creepf | 104.3 | 2 | – | 2870 | 410 | 14 | |
Olivine (dry) | Diffusion creepd | 109.2 | 1 | 3 | – | 375 | 4 |
Dislocation creepe | 106.1 | 3 | – | – | 510 | 11 | |
Peierls creepf | 106.3 | 2 | – | 9600 | 510 | 11 |