Merge branch 'master' into release/3.0.0

docs/running_simulations.md

@@ -103,7 +103,7 @@ Users can chose to generate their input files through a Python wrapper, called `
 |      `D`      | Damage level = $1 - \frac{\mathrm{damaged~shear~modulus}}{\mathrm{intact~shear~modulus}}$<br /><br />This feature is currently implemented only for `MESHDIM = 1` and `FINITE = 0` |      `0`      |
 |     `HD`      | If `D > 0`, half-thickness of the fault damage zone (m)<br />If `D = 0`, half-thickness of an elastic slab bisected by a fault<br /><br />This feature is currently implemented only for `MESHDIM = 1` and `FINITE = 0` |      `0`      |
 |      `L`      | If `MESHDIM = 1`, `L` is the fault length (or spatial period; m)<br />If `MESHDIM = 0`, `MU/L` is the spring stiffness |      `1`      |
-|   `FINITE`    | Boundary conditions when `MESHDIM=1`:<br />`0` = **Periodic fault**: the fault is infinitely long, but slip is spatially periodic with period `L`, loaded by steady displacement at distance `W` from the fault.<br />`1` = **Finite fault**: the fault is infinitely long, but only a segment of length `L` is explicitly governed by a [friction law](model_assumptions.html#fault-rheology). The remainder of the fault has steady slip at a rate `V_PL`. If running the code with this option gives the error message `kernel file qdyn/kernel_I.tab is too short`, you should create a larger kernel file with the MATLAB function `TabKernelFiniteFit.m`.<br />`2` = **Symmetric periodic fault**: like option `0`, but slip is symmetric relative to the first element.<br />`3` = **Symmetric finite fault**: like option `1`, but slip is symmetric relative to the first element. This can be used to simulate a free surface adjacent to the first element. |      `1`      |
+|   `FINITE`    | Boundary conditions when `MESHDIM=1`:<br />`0` = **Periodic fault**: the fault is infinitely long, but slip is spatially periodic with period `L`, loaded by steady slip beyond an out-of-plane seismogenic width `W` (see below) or by steady displacement at distance `HD` from the fault if `D = 0`.<br />`1` = **Finite fault**: the fault is infinitely long, but only a segment of length `L` is explicitly governed by a [friction law](model_assumptions.html#fault-rheology). The remainder of the fault has steady slip at a rate `V_PL`. If running the code with this option gives the error message `kernel file src/kernel_I.tab is too short`, you should create a larger kernel file with the MATLAB function `TabKernelFiniteFit.m`.<br />`2` = **Symmetric periodic fault**: like option `0`, but slip is symmetric relative to the first element.<br />`3` = **Symmetric finite fault**: like option `1`, but slip is symmetric relative to the first element. This can be used to simulate a free surface adjacent to the first element. |      `1`      |
 |      `W`      | Out-of-plane seismogenic width of the fault (m), only if `MESHDIM=1` and `FINITE=0`, following the "2.5D" approximation introduced in appendix A.2 of [Luo and Ampuero (2017)](http://dx.doi.org/10.1016/j.tecto.2017.11.006). **Note** that the approximation assumes that the grid size is `> W`. |      `50e3`      |
 |    `DIP_W`    | Fault dip angle (degree). This parameter is only used when `MESHDIM=2`. If depth-dependent, values must be given from deeper to shallower depth. |      `90`      |
 |  `Z_CORNER`   | Fault bottom depth (m; negative down)                        |      `0`      |