MEKOMETER MEASUREMENTS IN THE IMPERIAL VALLEY, CALIFORNIA

A network of about 130 bench marks, mostly about 800 m apart at road intersections and forming a continuous chain of quadrilaterals crossing the Imperial Valley in the vicinity of El Centro, has been measured three times, in 1971, 1973 and 1975. The instrument used was a Mekometer, a superior short-range electronic-distance-measuring (EDM) instrument having a sensitivity of 0.1 mm and a potential accuracy of better than 1 ppm. In 1975 the network was extended, particularly where it crosses the Imperial fault, to about 200 bench marks defining about 500 lines. For various reasons, it has not been possible to achieve standard errors of much less than 3 ppm in the distance measurements. Even so, about one line in three shows significant change at the 95% level in one or more of the three intervals 1971-1973, 1973-1975 and 1971-1975. Adopting stringent consistency criteria, the number of places where significant changes occurred can be reduced to seven. One of these is almost certainly associated with the Heber geothermal anomaly, one with the Imperial fault, and the others with one or other of the faults identified on the ground further to the north. The largest and most consistent changes occur on the Imperial fault, and imply an aseismic slip on it averaging about 8 mm/yr. The data also lend themselves to regional strain analysis. The results are consistent with a linear strain rate of about 0.3 ppm/yr, which is comparable with the rate deduced from large-scale geodetic surveys of the area. © 1979.