A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec.
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 inve...
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McGill University
1956
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ndltd-LACETR-oai-collectionscanada.gc.ca-QMM.1102562014-02-13T04:06:22ZA study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec.Marleau, Raymond. A.Geological Sciences.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.McGill UniversitySaull, V. (Supervisor)1956Electronic Thesis or Dissertationapplication/pdfenalephsysno: NNNNNNNNNTheses scanned by McGill Library.All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.Master of Science. (Department of Earth Sciences.) http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=110256 |
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en |
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Others
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Geological Sciences. |
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Geological Sciences. Marleau, Raymond. A. A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec. |
description |
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. |
author2 |
Saull, V. (Supervisor) |
author_facet |
Saull, V. (Supervisor) Marleau, Raymond. A. |
author |
Marleau, Raymond. A. |
author_sort |
Marleau, Raymond. A. |
title |
A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec. |
title_short |
A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec. |
title_full |
A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec. |
title_fullStr |
A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec. |
title_full_unstemmed |
A study of the relation of the Earth’s field as presented on aeromagnetic maps to the geology in Beauce area, Quebec. |
title_sort |
study of the relation of the earth’s field as presented on aeromagnetic maps to the geology in beauce area, quebec. |
publisher |
McGill University |
publishDate |
1956 |
url |
http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=110256 |
work_keys_str_mv |
AT marleauraymonda astudyoftherelationoftheearthsfieldaspresentedonaeromagneticmapstothegeologyinbeauceareaquebec AT marleauraymonda studyoftherelationoftheearthsfieldaspresentedonaeromagneticmapstothegeologyinbeauceareaquebec |
_version_ |
1716645198827618304 |