The phase relations in the Fe-As-S system at 600°0, studied in rigid silica glass tubes where a vapor phase is always present, are as follows: a liquid field extends along the S-As join from 100 to 22.8 +/- 0.2 weight per cent sulfur. An extensive pyrite-liquid-vapor field and a narrower pyrrhotite-liquid-vapor field are separated by the four-phase region pyrite-pyrrhotite-liquid-vapor in which the composition of the liquid is, in weight per cent, approximately As = 62.5, S = 37.5, and Fe = 0.11. [...]
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.111734 |
| Date | January 1959 |
| Creators | Clark, Lloyd A. |
| Contributors | Stevenson, J.S. (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 | Doctor of Philosophy. (Department of Geological Science.) |
| 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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