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TitleAn automatic 3-magnet or biastatic magnetometer
DownloadDownloads
AuthorChristie, K W; Larochelle, A
SourceGeological Survey of Canada, Paper 67-28, 1967, 28 pages, https://doi.org/10.4095/102968
Year1967
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceCanada; British Columbia; Alberta; Saskatchewan; Manitoba; Ontario; Quebec; New Brunswick; Nova Scotia; Prince Edward Island; Newfoundland and Labrador; Northwest Territories; Yukon; Nunavut
NTS1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65; 66; 67; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 84; 85; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114O; 114P; 115; 116; 117; 120; 340; 560
Subjectsgeophysics; magnetometers; paleomagnetism
Released1967 01 01; 2016 02 02
AbstractThe widely used 2-magnet, Blackett-type astatic magnetometer cannot be used efficiently for Palaeomagnetic research in laboratories where the ambient magnetic field and its vertical gradient are subject to constant variations. It is shown that under such conditions, the 3-magnet or "biastatic" magnetometer is theoretically more stable and adequate. Considerations for the design of such an instrument are briefly reviewed and a description is given of an instrument of this type developed at the Geological Survey of Canada, An important feature of this instrument is that its operation can be carried out automatically. The results obtained in testing the performance of the instrument are analyzed,
GEOSCAN ID102968