This thesis represents a general study of the geology of an area of approximately 140 square miles, situated in Ungava, New Quebec, which covers part of the eastern “contact” of the so called “Labrador Trough“ with the granite-gnei ss-migmatite complex. The study is based on field work carried out during the summers of 1954 and 1955 for the Quebec Department of Mines, and laboratory investigation at McGill University during 1955 and 1956. The abject of this paper is to prove that the rocks in that part of the "Labrador Trough” show progressive regional metamorphism towards the East and North.
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.110177 |
| Date | January 1956 |
| Creators | De Romer, Henry. S. |
| Contributors | Kranck, E. (Supervisor) |
| Publisher | McGill University |
| Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
| Language | English |
| Detected Language | English |
| Type | Electronic Thesis or Dissertation |
| Format | application/pdf |
| Coverage | Master of Science. (Department of Earth Sciences.) |
| Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
| Relation | alephsysno: NNNNNNNNN, Theses scanned by McGill Library. |
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