1967
DOI: 10.1190/1.1439897
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The Geomagnetic Gradiometer

Abstract: The geomagnetic gradiometer is a new geophysical prospecting tool which measures directly the vertical gradient of the earth’s magnetic field and the total field intensity. The system is composed of two simultaneously recording, optically pumped and monitored magnetometer sensors suspended from a helicopter. The sensors are separated vertically by a known distance so that the magnetic gradient can be determined from the difference in total magnetic intensity between the two sensors. Since the gradient is measu… Show more

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Cited by 61 publications
(18 citation statements)
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“…Typically, several indices are used, and the one that provides the best fit to known superficial geological structure, seismic data, boreholes, etc., or the one having good clustering properties is accepted. [On a possibility to estimate structural index, see Slack et al (1967), Steenland (1968), Barbosa et al (1999), and Martelet et al (2001)]. …”
Section: The Methods Of Euler Deconvolutionmentioning
confidence: 99%
“…Typically, several indices are used, and the one that provides the best fit to known superficial geological structure, seismic data, boreholes, etc., or the one having good clustering properties is accepted. [On a possibility to estimate structural index, see Slack et al (1967), Steenland (1968), Barbosa et al (1999), and Martelet et al (2001)]. …”
Section: The Methods Of Euler Deconvolutionmentioning
confidence: 99%
“…The derivatives of the total magnetic field can be determined using numerical procedures of Baranov (1975), Nabighian (1984) or with gradiometers (Slack et , 1967;Eggers and Thompson, 1984;Herwanger et al, 2000). Baranov (1975) presented coefficients for the numerical determination of vertical derivative of the potential fields.…”
Section: Prospecting Areamentioning
confidence: 99%
“…Gradiometers, measuring the difference in magnetic intensity between two sensors, make full use of the inherent sensitivity of high-resolution magnetometers. Slack et al (1967) gave an account of the first rubidium-vapor gradiometer. Gradient measurements have the great advantage of being independent of time variations of the magnetic field, since these are identical at the two sensors.…”
Section: Instrumentationmentioning
confidence: 99%