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国家地震局地质研究所在四川省西昌市邛海建成遥测地倾斜网并于1986年9月正式通过验收。 遥测地倾斜测网是观测地形变的一种新方法。它的工作原理与连通管倾斜仪一致,即根据两端仪表部分的液面升降确定相对地壳垂直形变量和倾斜方向。遥测地倾斜测网则是利用观测湖泊水平面的升降确定地壳的相对垂直形变量和倾斜方向。
Institute of Geology State Seismological Bureau in Xichang City, Sichuan Province, built a telemetry tilt grid and in September 1986 formally passed the acceptance. Telemetry tilt measurement network is a new way to observe the deformation of the terrain. Its working principle is the same as that of the connecting tube inclinometer, that is, the vertical deformation and the direction of inclination relative to the crust are determined according to the liquid level rise and fall of the instrument parts at both ends. Telemetric geodetic network is the determination of the relative vertical deformation and tilt direction of the crust by the elevation of the observed lake level.