|Title||Geodetic evidence for a blind fault segment at the southern end of the San Jacinto Fault Zone|
|Publication Type||Journal Article|
|Year of Publication||2018|
|Authors||Tymofyeyeva E., Fialko Y|
|Journal||Journal of Geophysical Research-Solid Earth|
|Type of Article||Article|
|Keywords||andreas fault; blind; california; fault; Geochemistry & Geophysics; GPS; hector mine earthquake; imperial-valley; InSAR; insar measurements; interseismic slip; San Jacinto fault; seismic-hazard; slip rates; strain rates; surface deformation; synthetic-aperture radar; volcanic rift zones|
The San Jacinto Fault (SJF) splits into several active branches southeast of Anza, including the Clark fault and the Coyote Creek fault. The Clark fault, originally believed to terminate at the southern tip of the Santa Rosa Mountains, was suggested to extend further to the southeast to a junction with the Superstition Hills fault based on space geodetic observations and geologic mapping. We present new interferometric synthetic aperture radar and GPS data that confirm high deformation rates along the southeastern extent of the Clark fault. We derive maps of horizontal and vertical average velocities by combining data from the ascending and descending satellite orbits with an additional constraint provided by the azimuth of the horizontal component of secular velocities from GPS data. The resulting high-resolution surface velocities are differentiated to obtain a map of maximum shear strain rate. Joint inversions of InSAR and GPS data suggest that the hypothesized blind segment of the Clark fault and the Coyote Creek fault have slip rates of 13 3mm/yr and 5 4mm/yr, respectively. The blind southern segment of the Clark fault thus appears to be the main active strand of the SJF, posing a currently unrecognized seismic hazard.