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An Assessment of the BGS δDδI Vector Magnetometer

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dc.creator Marsal, Santiago
dc.creator Torta, Joan Miquel
dc.creator Riddick, John C.
dc.date 2008-05-28T14:08:29Z
dc.date 2008-05-28T14:08:29Z
dc.date 2007
dc.date.accessioned 2017-01-31T01:29:18Z
dc.date.available 2017-01-31T01:29:18Z
dc.identifier Publs. Inst. Geophys. Pol. Acad. Sc., C-99 (398), 158-165, 2007
dc.identifier 0138-0117
dc.identifier http://hdl.handle.net/10261/4610
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/4610
dc.description Assuming optimal conditions, the δDδI vector magnetometer can be considered as a semi-absolute instrument. In this paper, the real situation and its differences with the ideal one are critically examined and regarded as potential sources of error. The analysis is applied to the equipment designed by the British Geological Survey (BGS) in the late 1980s, and the given figures are provided from the instrument in use at the Livingston Island Geomagnetic Observatory (LIV). Improved versions have been developed since then, being based on generally the same principles of measurement; thus, most of the results shown can be adapted to the new generation of magnetometers of this type.
dc.description Peer reviewed
dc.format 256353 bytes
dc.format application/pdf
dc.language eng
dc.publisher Polish Academy of Sciences
dc.rights openAccess
dc.source http://pub.igf.edu.pl/index.php?action=showarticles&series=C&pub_id=96
dc.subject Vector magnetometers
dc.subject Geomagnetism
dc.title An Assessment of the BGS δDδI Vector Magnetometer
dc.type Artículo


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