Abstract
Platinum-rich midcrustal and zoned intrusive complexes in the Fifield district make up part of a broad zone of Late Ordovician shoshonitic igneous rocks which crop out over a wide area of the eastern Lachlan fold belt. By studying the oxygen isotope fractionation between minerals in the Fifield intrusions, the significance of various magmatic processes is assessed. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1831-1840 |
| Number of pages | 10 |
| Journal | Economic Geology |
| Volume | 90 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - 1995 |
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Dive into the research topics of 'Oxygen and hydrogen isotope evidence for the origin of platinum- group element mineralization in Alaskan-type intrusions at Fifield, Australia'. Together they form a unique fingerprint.Cite this
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