Many orebodies have been formed in low temperature environments, distant from any known source and beyond the influence of ground water. These facts imply that ore metals travel in some way from a source to the places where they are found. Various theories have been put forward which purport to explain how this may happen. Because metals and their common silicates and sulphides are, with a few exceptions, volatile only at temperatures considerably above the temperatures at which epithermal deposits are thought to form, most theories postulate the presence of water to act as a moving flux in which the ore constituents are carried along.
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111289 |
| Date | January 1957 |
| Creators | Relly, Bruce. H. |
| Contributors | Saull, V. (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. |
Page generated in 0.002 seconds