Magnetic Data Reduction of Basement Correction

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dc.contributor.authorBadugama, L.N.
dc.contributor.authorCooray, J.T.
dc.date.accessioned2022-03-09T03:43:15Z
dc.date.available2022-03-09T03:43:15Z
dc.date.issued2013
dc.description.abstractThe magnetometer survey is a passive geophysical technique that measures the contrasts of magnetic properties between the feature of interest and its surrounding environment. This technique has wide applications in mineral and archeological investigations. Rocks and minerals with high ferrous content provide anomalous signatures than the background enabling to screen them. The magnetometer surveys are always disturbed by temporal variations: Diurnal variation, Magnetic storms and Micro-pulsation, which depend upon the time and space. Magnetic surveys are not done during magnetic storms. The diurnal variation cannot be avoided and the noise will disturb the data quality. To eliminate the diurnal variation from data a base station is used in magnetic surveys. In order to overcome the temporal variations, a base magnetometer is needed to correct these time dependent variations. . While the base records the temporal variation of the area the rowing magnetometer records both the temporal variation and the local anomaly. For a large-area survey, or an airborne survey, the magnetic field may be monitored at several locations, continuously, to identify the spatial variations of the time-varying field. If the rover is too far away from the base station, the time-varying fields measured at the rover will differ from those measured at the base station, resulting in increased error. The effective range of a single base station is generally considered to be less than 100 km for air-borne survey and for a ground survey it is about 200 m. This distance may vary according to the survey area and the expected accuracy. Owing to the large area covered by an aeromagnetic survey, a single magnetic base station would not have provided adequate coverage. Instead, several base station magnetometers are in operation during the survey (Hrouda et al, 2009). The base correction is conducted with the assumption that the environmental effects over the survey area are constant. The base magnetometer is synchronized with the rowing component and the environmental effect is removed according to the respective time stamps. However, if the survey area is large, the base station needs to be shifted as the assumption is no longer valid. As the crustal magnetic component of locations where the base station(s) establish during a survey is not a constant, a correction is needed to be applied for base stations. The present work attempts formulating a model for the basement correction. Methodology A mathematical model that completely describes the magnetic surveys, with two sub surveys was created. This method can be extended for many sub surveys, considering two sub surveys at a time. The variables were: IGRF value, local anomaly, environmental noise, local anomaly at the base station, and the location.en_US
dc.identifier.urihttp://www.erepo.lib.uwu.ac.lk/bitstream/handle/123456789/8479/03-MRT-Magnetic%20Data%20Reduction%20of%20Basement%20Correction%20.pdf?sequence=1&isAllowed=y
dc.language.isoenen_US
dc.publisherUva Wellassa University of Sri Lankaen_US
dc.subjectMineral Sciencesen_US
dc.subjectMineralen_US
dc.subjectGeographic Information Systemen_US
dc.subjectGeophysicalen_US
dc.titleMagnetic Data Reduction of Basement Correctionen_US
dc.title.alternativeResearch Symposium 2013en_US
dc.typeOtheren_US
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