Application of collocation for the planning of gravity surveys

Details Application of collocation for the planning of gravity surveys Application of collocation for the planning of gravity surveys

Jun 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975bgeod..49..183t&link_type=abstract

Bulletin Géodésique, Volume 49, Issue 2, pp.183-198

Astronomy and Astrophysics

Astronomy

6

Scientific paper

Least squares collocation can be used to determine the density of a gravity survey, when the object of the survey is:
1.
To produce a (free-air) gravity anomaly map, so that point gravity anomaly values can be interpolated with a standard error of ±X1 mgal,
2.
To interpolate deflections of the vertical with a standard error of ±X2 arc. sec. between astronomical stations Z km apart,
3.
To compute an upward continuation of a point gravity anomaly to a height of Z meters with a standard error of ±X3 mgal,
4.
To compute mean gravity anomalies of block size Z degrees with a standard error of ±X4 mgal,
5.
To obtain a (local) gravimetric geoid with a standard error of ±X5 meters,
6.
To compute density anomalies at a depth of Z km with a standard error of ±X6 g/cm3.

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