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AssigneeCommissariat a l'Energie Atomique
InventorsJacques Pocachard, Veronique Barthes
Estimating the term…
Probe and process for measuring the remanent field (R) of a geological formation. A measurement is made of the magnetic field (B+I1+R1) along the axis of the geomagnetic field using a scalar magnetometer, followed by a vector measurement of the resultant magnetic field (Bp+Ip+R3) projected onto an invariable measurement axis. With the aid of the calculated values of the geomagnetic field (B) and the magnetic susceptibility field (I), it is in particular possible to calculate a component (S) of the remanent magnetic field (R) perpendicular to the geomagnetic field (B) and determine if the cancellation of the component of the field (R1) along this axis is due to a tilting of the magnetic pole in history or a local reduction of the remanent magnetization.
Installation for detecting a component (S) of a remanent field (R), associated with a remanent magnetization, of a geological formation also having a magnetic susceptibility associated with a magnetic susceptibility field (I), the geological formation being submerged in a geomagnetic field (B), the geomagnetic, remanent and susceptibility fields forming a total magnetic field in a direction of the geomagnetic field, the detected component (S) of the remanent field (R) being secant to the direction of the geomagnetic field, said installation comprising a scalar magnetometer (7), located at a measurement site in the geological formation, for measuring the total magnetic field in the direction of the geomagnetic field, means, located at a surface site generally above the geological formation, for measuring the geomagnetic field (B) in intensity and direction at the geological formation, means, located at the measurement site in the geological formation, for measuring the magnetic susceptibility field (I) in intensity and direction, a second magnetometer (8, 8'), located at the measurement site in the geological formation, for measuring an algebraic sum of the geomagnetic, remanent and susceptibility fields projected in a measurement direction differing from the direction of the geomagnetic field, and means, in communication with the scalar magnetometer, the geomagnetic field measuring means, the magnetic susceptibility field measuring means, and the second magnetometer, for calculating the component (S) of the remanent field as a function of the total magnetic field in the direction of the geomagnetic field, the intensity and direction of the geomagnetic field, the intensity and direction of the magnetic susceptibility field, and the algebraic sum of the geomagnetic, remanent and susceptibility fields projected in the measurement direction.
Process for detecting a remanent field (R), associated with a remanent magnetization, of a geological formation also having a magnetic susceptibility associated with a magnetic susceptibility field (I), the geological formation being submerged in a geomagnetic field (B), the geomagnetic, remanent and susceptibility fields forming a total magnetic field in a direction of the geomagnetic field, said process comprising the steps of measuring the total magnetic field in the direction of the geomagnetic field at a measurement site in the geological formation, obtaining in direction and intensity the geomagnetic field (B) and the magnetic susceptibility field (I), measuring an algebraic sum of the geomagnetic, remanent and susceptibility fields at the measurement site in the geological formation in a measurement direction differing from the direction of the geomagnetic field, obtaining an angle between the measurement direction and the total magnetic field direction, calculating components (Bp, Ip) of the geomagnetic field and the magnetic susceptibility field along the measurement direction as a function of the angle between the measurement direction and the total magnetic field direction, the intensity of the geomagnetic field, and the direction and intensity of the magnetic susceptibility field, and calculating a component (R3) of the remanent magnetic field (R) along the measurement direction as a function of the algebraic sum of the geomagnetic, remanent and susceptibility fields in the measurement direction, and the components of the geomagnetic field and the magnetic susceptibility field along the measurement direction.
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