The airborne magnetometer was developed during World War II as a submarine detector, and is now a standard tool of modern geophysics. Since its development, the airborne magnetometer has helped locate valuable ore deposits, it has aided to decipher geological structures, and it has been used to investigate the possible future activity of volcanoes. Airborne magnetic surveys are not essentially different from land magnetic surveys: aeromagnetic data are obtained and compiled along a continuous line, whereas ground magnetic surveys are made at separate points.
Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.110256 |
Date | January 1956 |
Creators | Marleau, Raymond. A. |
Contributors | Saull, V. (Supervisor) |
Publisher | McGill University |
Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
Language | English |
Detected Language | English |
Type | Electronic Thesis or Dissertation |
Format | application/pdf |
Coverage | Master of Science. (Department of Earth Sciences.) |
Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
Relation | alephsysno: NNNNNNNNN, Theses scanned by McGill Library. |
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