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http://hdl.handle.net/11375/18959
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DC Field | Value | Language |
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dc.contributor.advisor | Clifford, P. M. | - |
dc.contributor.author | Hennessey, B. Terrence | - |
dc.date.accessioned | 2016-03-15T19:20:04Z | - |
dc.date.available | 2016-03-15T19:20:04Z | - |
dc.date.issued | 1979-04 | - |
dc.identifier.uri | http://hdl.handle.net/11375/18959 | - |
dc.description.abstract | <p> A syncline-anticline pair in miogeosynclinal sediments of the western margin of the Labrador Trough was mapped. Samples were taken of each rock unit and a structural analysis was performed. The structure determined was compared in an elementary fashion to geophysics completed over the mapping area. </p> <p> The folds in the pair are highly variable along their length changing from an open to tight folding style and with a rolling plunge varying from 3° NW to 12° SE. </p> <p> The beds of the folds show no internal deformation except for drag folding in the shaly units. The rocks were folded by a flexural slip mechanism. </p> <p> The gravity and ground magnetics successfully outlined the structure of the fold, dipping of the beds and in one instance located a fault. Typical gravity values (signatures) for a number of rock units are easily determined.</p> | en_US |
dc.language.iso | en | en_US |
dc.subject | Labrador Trough | en_US |
dc.subject | anticline | en_US |
dc.subject | Schefferville | en_US |
dc.subject | Schefferville | en_US |
dc.subject | rock | en_US |
dc.title | A Structural Analysis of an Anticline-Syncline Pair in the Labrador Trough Near Schefferville, P. Q. | en_US |
dc.type | Thesis | en_US |
dc.contributor.department | Geology | en_US |
dc.description.degreetype | Thesis | en_US |
dc.description.degree | Bachelor of Science (BSc) | en_US |
Appears in Collections: | Bachelor theses |
Files in This Item:
File | Description | Size | Format | |
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Hennessey_B_Terrence_1979Apr_BSc.pdf | Thesis | 15.65 MB | Adobe PDF | View/Open |
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