Opaque mineral assemblage formed during serpentinization in the Coolac ultramafic belt, New South Wales
- 1 January 1975
- journal article
- Published by Taylor & Francis in Journal of the Geological Society of Australia
- Vol. 22 (1), 91-102
- https://doi.org/10.1080/00167617408728877
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Petrogenesis of sulphide-bearing reaction zones in the Coolac ultramafic belt, New South Wales, AustraliaMineralium Deposita, 1973
- Some replacement phenomena in copper-nickel sulphide oresMineralium Deposita, 1971
- A Chemical Study of Serpentinization--Burro Mountain, CaliforniaJournal of Petrology, 1971
- A microprobe study of chromites from the Andızlık-Zımparalık area, south-west TurkeyMineralogical Magazine, 1971
- Petrologic and Geophysical Nature of SerpentinitesGSA Bulletin, 1971
- Serpentinisation of harzburgites from the alpine peridotite belt of Southwest TurkeyChemical Geology, 1970
- The Relationship between Fluids in Some Fresh Alpine-Type Ultramafics and Possible Modern Serpentinization, Western United StatesGSA Bulletin, 1969
- SULFIDES IN THE MUSKOX INTRUSIONCanadian Journal of Earth Sciences, 1967
- NATIVE METALS IN THE MUSKOX INTRUSIONCanadian Journal of Earth Sciences, 1965
- Wairauite—a new cobalt-iron mineralMineralogical Magazine and Journal of the Mineralogical Society, 1964