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| | Calculating Bouguer Anomalies from Observed Gravity Values (Site not responding. Last check: 2007-10-09) |
 | | The process involved calibrating the data, applying tidal corrections, averaging repeated values and their times of occupation, dedrifting the values, obtaining gravity differences between the base and the stations referred to it, and finally converting the relative values to absolute values using a base at which absolute gravity is known. |
 | | The Bouguer anomaly is named after a French scientist (Pierre Bouguer), who derived the formula for an infinitely extending slab, the basis for the so-called mass correction (discussed below). |
 | | Two types of Bouguer anomalies are recognized: (1) simple Bouguer anomalies, in which the various factors have been corrected, with the exception of terrain effects, and (2) complete Bouguer anomalies, for which terrain effects have also been removed. |
| seis.natsci.csulb.edu /grannell/secondgravity.html (1285 words) |
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