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dc.contributor.author Mandziuk, William Stanley en_US
dc.date.accessioned 2009-12-03T19:18:48Z
dc.date.available 2009-12-03T19:18:48Z
dc.date.issued 1989-08-01-01:09T00:00:00Z en_US
dc.identifier ocm72736855 en_US
dc.identifier.uri http://hdl.handle.net/1993/3645
dc.description.abstract The Falcon Lake Intrusive Complex is a composite intrusive body, approximately 10 square kilometers in area, located near the western edge of the Wabigoon Subprovince in the Superior Province of the Canadian Precambrian Shield. The complex has an elliptical shaped core, and tapering extensions to the southwest and northeast. The complex consists of a series of intrusions ranging from oldest gabbroic rocks in the extensions, through younger diorite-granodiorite in the outer areas of the core, to youngest quartz monzonite in the centre. All of the rocks of the complex are characterized by cumulate or porphyritic textures. The compositions, distribution, and relative ages of the component intrusions suggest a, separate differentiating magma chamber from which the intrusions were drawn sequentially. Successive intrusions of progressively more differentiated magma were intruded more or less into the centre of its less differentiated predecessor. The initial intrusion was dyke-like, and succeeding intrusions gave the complex a more equant and cylindrical shape. Relationships throughout the complex suggest that the complex was a magma conduit in which magmas were periodically transported from a source at depth to higher level intrusive or extrusive features. Each intrusion of the complex is characterized by its own set of primary fabric structures which may include the preferred orientation of primary minerals, layering, discordant intrusive contacts similar to angular unconformities, scour and trough-banded structures, mineral clots and segregations of various compositions, xenoliths and cognate inclusions, and breccia pipes. The form and arrangement of these primary structures. as well as relationships between structures, suggest that each intrusion initially consisted of a crystal-liquid mixture, and that magmatic flow processes were responsible for the development of the structures. The origin of the flow is related to intrusive emplacement mechanisms rather than convection processes after emplacement. en_US
dc.format.extent vii, 103 leaves : en_US
dc.format.extent 17653323 bytes
dc.format.mimetype application/pdf
dc.language en en_US
dc.language.iso en_US
dc.rights The reproduction of this thesis has been made available by authority of the copyright owner solely for the purpose of private study and research, and may only be reproduced and copied as permitted by copyright laws or with express written authorization from the copyright owner. en_US
dc.title Primary structures of the Falcon Lake Intrusive Complex, southeastern Manitoba en_US
dc.degree.discipline Geological Sciences en_US
dc.degree.level Master of Science (M.Sc.) en_US


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