Table 1 Experimental setting for dry dunite deformation from Chopra and Paterson (1984). All the stress-versus-strain series are available from their supplementary material. The initial conditions used to solve the ordinary differential equation for the MCMC inversion and the best-fit model are provided here
Run number | T (K) | \({\dot{\varepsilon }}\) in \(\hbox {s}^{-1}\) | \(\sigma (0)\) | \(\varepsilon _\mathrm {M}(0)\) | \(\varepsilon _\mathrm {K}(0)\) | \(\varepsilon (0)\) |
|---|---|---|---|---|---|---|
4580 | 1673 | 1.0 × 10\(^{-4}\) | 0 | 0 | 0 | 0 |
4580 | 1673 | 3.2 × 10\(^{-5}\) | 190 | 3.52 | 0.58 | 4.1 |
4580 | 1673 | 9.9 × 10\(^{-6}\) | 138 | 6.67 | 0.43 | 7.1 |
4469 | 1573 | 1.1 × 10\(^{-4 }\) | 0 | 0 | 0 | 0 |
4469 | 1573 | 1.0 × 10\(^{-5}\) | 131 | 7.69 | 0.01 | 7.7 |
4469 | 1573 | 1.1 × 10\(^{-4}\) | 229 | 8.93 | 0.67 | 9.6 |
4526 | 1483 | 5.3 × 10\(^{-5}\) | 0 | 0 | 0 | 0 |
4675 | 1483 | 1.2 × 10\(^{-5}\) | 0 | 0 | 0 | 0 |
4675 | 1483 | 1.3 × 10\(^{-6}\) | 389 | 4.53 | 1.17 | 5.7 |
4461 | 1463 | 1.1 × 10\(^{-5}\) | 0 | 0 | 0 | 0 |
4581 | 1573 | 1.1 × 10\(^{-4}\) | 0 | 0 | 0 | 0 |
4581 | 1573 | 3.3 × 10\(^{-5}\) | 368 | 3.95 | 1.15 | 5.1 |
4581 | 1573 | 1.0 × 10\(^{-5}\) | 271 | 7.18 | 0.82 | 8.0 |
4666 | 1483 | 3.6 × 10\(^{-5}\) | 0 | 0 | 0 | 0 |
4666 | 1483 | 3.7 × 10\(^{-6}\) | 470 | 5.9 | 1.5 | 7.4 |
4668 | 1483 | 9.7 × 10\(^{-6}\) | 0 | 0 | 0 | 0 |
4668 | 1483 | 1.1 × 10\(^{-6}\) | 348 | 1.5 | 1.1 | 2.6 |
4667 | 1483 | 3.1 × 10\(^{-5}\) | 0 | 0 | 0 | 0 |
4667 | 1483 | 3.4 × 10\(^{-6}\) | 567 | 5.6 | 1.7 | 7.3 |
4576 | 1573 | 1.1 × 10\(^{-4}\) | 0 | 0 | 0 | 0 |
4462 | 1473 | 1.2 × 10\(^{-5}\) | 0 | 0 | 0 | 0 |
4506 | 1553 | 1.2 × 10\(^{-4}\) | 0 | 0 | 0 | 0 |