Abstract
Rejects a statement by P. E. Hotz claiming that nickel silicate-type deposits of New Caledonia were formed on unserpentinized peridotite, concluding instead that the deposits lie on ultramafic rock that is largely serpentinized.
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
