The Paleoproterozoic structural history of metamorphosed and polydeformed basement and cover rocks in the Ptarmigan Fiord area, Baffin Island, Nunavut: a tectonic component of the Quebec-Baffin segment of the Paleoproterozoic Trans-Hudson orogen
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The structural geometry and Paleoproterozoic deformation history of the Ptarmigan Fiord area is based on mapping and structural analyses, integrated with published petrology and geochronology data. Early thrust repetition, of 80-200 m-thick sheets of Archean orthogneiss basement with Paleoproterozoic cover of the Lake Harbour Group, results in belts of basement-cover couplets. This was followed by DP2 penetrative transposition that occurred at amphibolite-facies at ca. 1850-1820 Ma. The major structure in the SE part of the map is an upright ~ NW- striking, tight F2b syncline that folded three basement-cover couplets. The fold has a wavelength of ~ 3 km, occurs over a strike length of ~ 11 km, and has been refolded. The NW part of the map area comprises a NW-dipping panel of basement rocks and three belts of basement-cover couplets. This NW-dipping panel was juxtaposed against the F2b syncline by a moderately NW-dipping, T3c reverse shear zone.
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Copyright © 2017 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner.
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