Skip to Main Content
Skip Nav Destination

The Malibu Coast Fault Zone (MCFZ) is an east-west-trending fault system that marks the southern boundary of the western Transverse Ranges along the Santa Monica Mountains of southern California. Focal mechanism solutions for 107 earthquakes in the study area are mostly associated with thrusts or thrust-dominated oblique faults with a small left-lateral component of strike slip. The average azimuth of hanging-wall slip is 206°, which is approximately perpendicular to the trace of the San Andreas fault through the Transverse Ranges. Approximately 60% of the inferred slip vectors had azimuths between 180° and 240°. Six ML ≥5 earthquakes have...

You do not currently have access to this chapter.

Figures & Tables

Contents

References

Related

Citing Books via

Close Modal

or Create an Account

Close Modal
Close Modal