Osmium isotope evidence for a crustal origin of platinum group elements in the Sudbury nickel ore, Ontario, Canada
- 1 September 1992
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 56 (9) , 3531-3537
- https://doi.org/10.1016/0016-7037(92)90396-z
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- Negative thermal ion mass spectrometry of osmium, rhenium and iridiumPublished by Elsevier ,2003
- Geochemical stratigraphy of the Huronian continental volcanics at Thessalon, Ontario: contributions of two-stage crustal fusionContributions to Mineralogy and Petrology, 1992
- Direct determination of the half-life of 187ReGeochimica et Cosmochimica Acta, 1989
- Assimilation and crystallization in basic magma chambers: trace-element and Nd-isotopic variations in the Kerns sill, Nipissing diabase province, OntarioCanadian Journal of Earth Sciences, 1989
- A “solid spike” method for Re-Os analysis of acid-resistant minerals enriched in platinumgroup elements (PGE)Chemical Geology, 1988
- Direct laboratory determination of the 187Re half-lifeNature, 1986
- Origin of the Sudbury Complex by Meteoritic Impact: Neodymium Isotopic EvidenceScience, 1985
- Neodymium isotopes in the Colorado Front Range and crust–mantle evolution in the ProterozoicNature, 1981
- The Age of the Sudbury Nickel Irruptive and the Murray GraniteCanadian Journal of Earth Sciences, 1975
- Sudbury Structure as an AstroblemeThe Journal of Geology, 1964