Summary
Small variations in the vertical component of gravity (gv have been found to be of considerable use in geophysical exploration. The phenomenon of interest to conventional exploration geophysics is the variation of gv with position on the surface. Two-dimensional contour maps of this variation are usually prepared. The change in gv caused by a buried mass will, of course, be greatest directly above the mass, but will vary with the horizontal distance between the mass and the measuring point. This variation can be used to attempt to locate and describe the mass. Surface gravimetry is typically used to locate buried faults, domes and other structures of interest to the exploration geophysicist, and a vast literature exists describing the method.
Borehole gravimetry is a fairly recent extension of surface gravimetry to the third dimension. The phenomenon of interest is the variation of gv with depth in the hole. This variation, like that on the surface, is caused by both the vertical and lateral position of the buried mass, but while with the surface gravimeter the lateral distance between the mass of interest and the instrument is changed, with the borehole gravimeter the vertical distance is changed instead. This permits a different look at the mass and a somewhat different method of analysis.
This paper discusses the history of the development of borehole gravimetry and the borehole gravimeter. Important aspects of field operations are described and the corrections necessary for data reduction are explained. The several methods of analysing the data to attempt to infer subsurface structure from borehole gravity and density log data are outlined. Finally, a number of applications of the method are listed.
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Hearst, J.R., Carlson, R.C. (1982). Measurement and Analysis of Gravity in Boreholes. In: Fitch, A.A. (eds) Developments in Geophysical Exploration Methods—3. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-7349-7_8
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