The S-isotopic compositions of sulfide deposits from Steinmann, granitoid and felsic volcanic associations have been examined. Ores of Steinmann association have 8~'S values close to zero per rail (8~S = +0.3 + 3.1%o); it appears they are of mantle origin. Isotopically, ores of granitoid associatio
Sulfur isotopes and the origin of stibnite mineralisation in New England, Australia
โ Scribed by Brian W. Robinson; Michael G. Farrand
- Publisher
- Springer
- Year
- 1982
- Tongue
- English
- Weight
- 869 KB
- Volume
- 17
- Category
- Article
- ISSN
- 0026-4598
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