Oxygen and hydrogen isotope evidence for the origin of platinum- group element mineralization in Alaskan-type intrusions at Fifield, Australia

A. S. Andrew; B. J. Hensen; A. C. Dunlop; P. D. Agnew

doi:10.2113/gsecongeo.90.6.1831

Oxygen and hydrogen isotope evidence for the origin of platinum- group element mineralization in Alaskan-type intrusions at Fifield, Australia

A. S. Andrew, B. J. Hensen, A. C. Dunlop, P. D. Agnew

Research output: Contribution to journal › Article › peer-review

10 Citations (Scopus)

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	https://doi.org/10.2113/gsecongeo.90.6.1831
Publication status	Published - 1995

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10.2113/gsecongeo.90.6.1831

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AU - Agnew, P. D.

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Oxygen and hydrogen isotope evidence for the origin of platinum- group element mineralization in Alaskan-type intrusions at Fifield, Australia

Abstract

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