SECONDARY FAULTS AND SLIP SENSE ALONG THE FRENCHMAN MOUNTAIN FAULT, SOUTHERN NEVADA
In some exposures, the FMF places Quaternary alluvial fan deposits in the hangingwall against Precambrian metamorphic basement rocks. The footwall basement rocks are tremendously faulted and sheared. The measured strikes of >100 minor footwall faults mostly range from N40oW to N40oE. They are primarily dip-slip faults, but some have minor strike-slip components. These faults are typically non-planar; many have ramp-flat geometries. Most fault sections dip between 30oW and vertical, but a few dip as gently as 5oW. The geometries appear to be controlled by competency contrasts between schist and gneiss within the basement. Also, the range of fault orientations might be a result of changes in geometry of the FMF throughout its development. Analysis of the footwall faults shows that (1) many are similar in orientation to the FMF and (2) others are Riedel shears, including R, R' and P shears.
In addition, 31 kinematic indicators were measured. Most are slickenlines and slickenfibers. The majority trend between N60oW and S50oW.
The Riedel shears, along with the other kinematic indicators, constrain the overall sense of slip along the FMF. The slip is generally normal (down-on-the-west), essentially dip slip, and the direction ranges from WNW to WSW.