For the Beijing Continuous GNSS stations, the site distances are small and
most of the stations are soil-based. The construction of the stations do not fully comply
with the earthquake monitoring standards and the crustal movement is in a very low
level. Considering all the above factors, we need study the feasibility to use the Beijing
Continuous GNSS stations for monitoring the crustal movement in Beijing. In this
paper, we carried out some preliminary study on respects of error, disturbance, point,
line and area based on a decade observational data. The results show that, the error can
be controlled by reasonable data processing methods and abandoning observations
with large error. By identifying and excluding some interference, we carried out
the site displacement analysis and found out the development process before and
after the Tokyo 8.0 earthquake. By analyzing the changing of the baselines between GNSS stations we acquired the movement characteristics of two active fault. By
analyzing the area changing, we realized some relationship among the area changing,
comprehensive Precursory information and mean moving rate of the faults. According
to the preliminary results, we think the Continuous GNSS stations can be used for
earthquake monitoring in Beijing.