Left lateral, right lateral, normal, reverse
Assume we are given a reference point r and a normal n pointing from the “+”side to the ““side of a fault segment. How does one describe the motion of the fault?
Leftlateral and rightlateral
“In a leftlateral (rightlateral) fault, an observer on one of the walls will see the other wall moving to the left (right).” [J. Pujol, Elastic Wave Propagation and Generation in Seismology]
Assume we stand on the ““side and look towards the “+”side, then if the strike vector s points to left, we have a leftlateral motion (for a positive sliprate). We formalize “points to the left” with:
\(l:=u\times(n)\)
where u is the unit vector which points up (e.g. (0,0,1) for enu or (0,0,1) for ned).
In SeisSol, the strike vector is (not normalized)
\(s:=(e_3)\times n\)
So, e.g., for enu we always have a leftlateral motion, as s and l are parallel, and for ned we always have a rightlateral motion as s and l are antiparallel.
Normal and reverse
“The foot wall (hanging wall) is defined as the block below (above) the fault plane. (…) the hanging wall moves up with respect to the foot wall and the fault is known as reverse. (…) the opposite happens and the fault is said to be normal.” [J. Pujol, Elastic Wave Propagation and Generation in Seismology]
In SeisSol, the dip vector is (not normalized)
\(d:=n\times s=n\times(e_3\times n)=e_3+n_zn\)
We used Grassmann’s Identity for the last step. In particular, we observe that the dip vector d is independent of the reference point, as we obtain the same vector for n and, as n is normalized and
\(d_z:=e_3+n_z^2\),
the dip vector always points in z direction. That is, the “+”side moves down for enu and the “+”side moves up for ned (assuming positive slip rate).
Normal or reverse depends also on the reference point. If the reference point is inside the hanging wall (foot wall) the “+”side corresponds to the hanging wall (foot wall).
In summary, we obtain the following table
foot wall= + 
hanging wall = + 


z = up 
reverse 
normal 
z = down 
normal 
reverse 
or logically
\(\text{isNormal}:=(+=\text{hanging wall})\leftrightarrow(z=\text{up})\)
Example
We have a 60° dipping normal fault with 90° strike (WestEast direction, pointing towards the East with enu convention) and 0° rake. The normal of the fault plane, which points from the foot wall to the hanging wall, is given by
\(n:=\frac{1}{2}\begin{pmatrix}0 & \sqrt{3} & 1\end{pmatrix}\)
Such normal vector is obtained as the result of the cross product between the dip vector
\(d:=\frac{1}{2}\begin{pmatrix}0 & 1 & \sqrt{3}\end{pmatrix}\)
and the respective strike vector
\(s:=\begin{pmatrix}1 & 0 & 0\end{pmatrix}\)
Hence, we set the reference point to x + a N, where a > 0 and x is an arbitrary point on the fault. In this case, the reference point is inside the hanging wall and we obtain a normal fault.
Warning
The rake angle describes the direction of slip. In SeisSol, the convention for the rake angle is to assume a positive rake angle refers to rightlateral strike slip. !Warning! This is opposite to the common convention in seismology which assumes positive rake angle implying leftlateral strike slip faulting. Thus, e.g., the case of Ts0>0 and Td0=0 means initial shear stress loading in rake 180° direction.