The mineralogy of the chrome spinels of the Bird River Sill, Manitoba
Hermatite exsolves from specimens of the Bird River chromite on heating. Exsolution begins in iron-rich areas, such as the rims of crystals and marginal to fractures where deuteric alteration of the chromite has occurred. With prolonged heating, exsolution extends throughout the crystals; optimum h...
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| Published: |
2012
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| Online Access: | http://hdl.handle.net/1993/5387 |