Map and list of reported occurrences of platinum-group metals in the conterminous United States
No abstract available.
Geology topics
Publications and source records attributed to N.J. Page.
No abstract available.
Some of the olivine cumulates of the Ultramafic zone of the Stillwater Complex, Montana, are progressively altered to serpentine minerals and thompsonite. Lizardite and chrysotile developed in the cumulus olivine and postcumulus pyroxenes; thompsonite developed in postcumulus plagioclase. The detailed mineralogy, petrology, and chemistry indicate that olivine and plagioclase react to form the alteration products, except for H 2 O, without changes in the bulk composition of the rocks.
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Explore the source record for details and available documents.
Explore the source record for details and available documents.
No abstract available.
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