found an error in how EQRM calculates the distances used by some GMPEs.
For deep faults (i.e. depth > than a fault width) there is a marked offset of
the area of hazard from the epicentre of the fault. What I think is happening
is where many GMPEs use the distance from a site to the nearest point of the
surface projection of the fault (i.e. vertically above the fault) EQRM seems to
be using the projection of the fault up the fault plane. So for a 45 degree
dipping fault the surface projection is being horizontally offset by the depth
of the hypocentre. This suggests to me, that the problem is most likely with
the function that calculates the Joyner-Boore distance.
I have run tests for six GMPEs and found the error in:
Atkinson06_bc_boundary_bedrock; Campbell08; Chiou08; and Sadigh_97.
The error does not appear to be in Somerville09_Non_Cratonic or
Toro_1997_midcontinent. Though Toro_1997_midcontinent appears to have no depth
dependency.
Original issue reported on code.google.com by duncan.g...@gmail.com on 11 Mar 2015 at 11:11
Original issue reported on code.google.com by
duncan.g...@gmail.com
on 11 Mar 2015 at 11:11