The Deweras Formation between the Umfuli and Umniati Rivers consists of an upper series of arkoses and shales, (Arenaceous Series), a middle sequence of tholeiitic lavas, (Volcanic Series), and a lower discontinuous series of quartzite and conglomerate, (Basal Sedimentary Series). The succession is interpreted as being deposited in a variable shallow water to continental environment, which in this instance is believed to be associated with a step faulted or graben structure. [...]
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.116800 |
| Date | January 1965 |
| Creators | Bliss, Neil Welbourne. |
| 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 Geological 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. |
Page generated in 0.0018 seconds