01.08.2021 | History

2 edition of Bouger anomaly map : Sudbury Ontario. found in the catalog.

Bouger anomaly map : Sudbury Ontario.

a sociological perspective

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Published by Administrator in Natural Resources Canada

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      • Filed with GSC serials11

        StatementNatural Resources Canada
        PublishersNatural Resources Canada
        LC Classificationsnodata
        The Physical Object
        Paginationxvi, 57 p. :
        Number of Pages70
        ID Numbers
        ISBN 10nodata
        2Canada.Geological Survey.Map 138

        nodata File Size: 1MB.

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Bouger anomaly map : Sudbury Ontario. by Natural Resources Canada Download PDF EPUB FB2

The SIC is believed to be a stratified impact melt sheet composed from the base up of sub layer norite, mafic norite, felsic norite, quartz gabbro, and granophyre. is the free-air gravity anomaly.


There are only a few samples that indicate these shock metamorphic features, none of which were found in their natural or original position or place Eyles 2002. 6 mgal a What does the positive Bouguer anormally reveal about the density of the ore body! Specific Features: The crater is occupied by a lake with a semi-circular north-shore, and defines a circle 8.

In the mid background is the rugged north eastern rim of the SIC Robertson et al 1975. It is classified as a simple meteorite crater because of its estimated diameter of 3 km E. General Area: Wanapitei is superimposed upon the eastern margin of the older, larger Sudbury structure. Subject: This map service provides access to Gravity Bouger Anomaly dataset shown on the GeoAtlas application. The Wanapitei impact happened over 1. It indicated a circular low approximately 2. Level ID: 8 [, ] Resolution: 611.

Footwall rocks, associated with the impact event, consist of Sudbury Brecciafootwall breccia, radial and concentric quartz dioritic breccia dikes polymict impact melt brecciasand the discontinuous sub layer. Science Training History of the Apollo Astronauts. Bouger anomaly map : Sudbury Ontario.

billion years ago in the era. Geological Society of America, Special Paper 384 2005 Canada. 2 points d What is the excess mass of the deposit? The contour interval is 0.