Presentation 1
Geophysics. GRAVIMETERY METHOD
Gravity Modeling 3
Problem 1 The corrections can be larger than the anomaly Stat.Time T Dist. (m) Elev. (m) Reading (dial units) Base reading at time T Drift corr’d anom.
Gravity Summary
By: Hamizah Hanim Hamzah, Helen Ellwood, and Zolt á n Erd ő s
By: Hamizah Hanim Hamzah, Helen Ellwood, and Zoltán Erdős.
Pengolahan Data Gravity
Figure and Gravity
