’ CIRES, University of Colorado/NOAA Boulder, Cola. (U.S.A.) ’ U.S. Geological Survey, Menlo Park, Calit (U.S.A.) (Received
March
10, 1983)
ABSTRACT
We installed a precise geodetic network along the San Andreas Pearblossom, California in November, 1980. The network is within frequently
referred
from a central measured (MWDM) protective
to as the “Palmdale
benchmark.
Uplift”
and consists
of 13 lines radiating
The lines range in length from 3.2 to 8.1 km are generally
several times each instrument is located shelter. The MWDM
week. The multiwavelength distance measuring at the central benchmark and is housed in a small instrument has demonstrated a capability to make
measurements to a precision of 1 part in 10 million. Using a coordinate system whose x-axis is parallel Andreas fault the following this effort: iXX = -0.180
k 0.025 pstr/yr
ivv = -0.031
_+0.029 pstr/yr
i,J’ = +0.077
+ 0.024 pstr/yr
A = -0.213
fault near the region
strain rates were observed
to the local trace of the San during
the first 10 months
of
f 0.039 pstr/yr
The observed strain rates do not appear to be constant in time, much of the deformation occurs in fairly well defined episodes. These changes in strain rate are particularly obvious in the iYv component.