The size distribution of heavy minerals in water-laid sediments has previously been explained in terms of the same fluvial sorting which controlled the grain size of the light minerals. What appeared to be a sympathetic variation between the size of heavy minerals and that of the light mineral with which they were associated led to the formulation of the concept of Hydraulic Equivalence and to belief in the constancy of the hydraulic ratio. [...]
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.117870 |
| Date | January 1965 |
| Creators | Longe, Robert Vernon. |
| Contributors | Mountjoy, 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 Geology.) |
| 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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