138 K. YE, Veselov and V. L. Panteleyev 



obvious that the use of sufficiently accurate gyroscopic stabilization for 

 a damped gravity measuring device with a horizontal torsion thread makes 

 highly accurate observations possible even for amplitudes of the accelerations 

 of 10-20 gal. This, at the same time, leads to the introduction of a minimum 

 number of corrections arising from the measurements. 



REFERENCES 



1. F. L. Vening Meinesz, Gravimetric observations at sea. Theory and practice. Geo- 



dezizdat, 1940. 



2. K. Ye. Veselov, The static method of measuring the force of gravity at sea. Priklad- 



naia geofizika, fasc. 15 Gostoptekhizdat (1956). 



3. L. V. SoROKiN, Gravimetry and gravimetric prospecting. Gostoptekhizdat, 1951. 



