A geophysical interpretation of structural boundaries in the Eastern Canadian Shield

Between 1958 and 1965 field parties of the Dominion Observatory observed some 11,000 gravity stations in northern Quebec as part of a program to provide gravity stations at intervals of 10-15 km,throughout Canada. The measurements were carried out using float-equipped fixed wing aircraft and helicop...

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Main Author: Tanner, James Gordon
Published: Durham University 1969
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Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.585885
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spelling ndltd-bl.uk-oai-ethos.bl.uk-5858852016-08-04T03:45:33ZA geophysical interpretation of structural boundaries in the Eastern Canadian ShieldTanner, James Gordon1969Between 1958 and 1965 field parties of the Dominion Observatory observed some 11,000 gravity stations in northern Quebec as part of a program to provide gravity stations at intervals of 10-15 km,throughout Canada. The measurements were carried out using float-equipped fixed wing aircraft and helicopters for transportation. The gravity measurements have been made by establishing a control network throughout northern Quebec which served as a reference for the gravity traverses. Analysis of the results indicates that the computed Bouguer anomalies in the northern part of the region are accurate to better than 3 mgal and those in the south to better than 2 mgal. The major source of error in the Bouguer anomalies is the uncertainty of the elevations of the gravity stations, most of which have been established using altimeters.557.1Durham Universityhttp://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.585885http://etheses.dur.ac.uk/8876/Electronic Thesis or Dissertation
collection NDLTD
sources NDLTD
topic 557.1
spellingShingle 557.1
Tanner, James Gordon
A geophysical interpretation of structural boundaries in the Eastern Canadian Shield
description Between 1958 and 1965 field parties of the Dominion Observatory observed some 11,000 gravity stations in northern Quebec as part of a program to provide gravity stations at intervals of 10-15 km,throughout Canada. The measurements were carried out using float-equipped fixed wing aircraft and helicopters for transportation. The gravity measurements have been made by establishing a control network throughout northern Quebec which served as a reference for the gravity traverses. Analysis of the results indicates that the computed Bouguer anomalies in the northern part of the region are accurate to better than 3 mgal and those in the south to better than 2 mgal. The major source of error in the Bouguer anomalies is the uncertainty of the elevations of the gravity stations, most of which have been established using altimeters.
author Tanner, James Gordon
author_facet Tanner, James Gordon
author_sort Tanner, James Gordon
title A geophysical interpretation of structural boundaries in the Eastern Canadian Shield
title_short A geophysical interpretation of structural boundaries in the Eastern Canadian Shield
title_full A geophysical interpretation of structural boundaries in the Eastern Canadian Shield
title_fullStr A geophysical interpretation of structural boundaries in the Eastern Canadian Shield
title_full_unstemmed A geophysical interpretation of structural boundaries in the Eastern Canadian Shield
title_sort geophysical interpretation of structural boundaries in the eastern canadian shield
publisher Durham University
publishDate 1969
url http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.585885
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