| Titre | Brucite: uses, exploration guidelines and selected grass-root exploration targets |
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| Auteur | Simandl, G L; Paradis, S; Irvine, M |
| Source | Canadian Institute of Mining Bulletin vol. 101, no. 1106, 2008, 7p.  Accès ouvert |
| Liens | Online - En ligne
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| Image |  |
| Année | 2008 |
| Séries alt. | Secteur des sciences de la Terre, Contribution externe 20100108 |
| Document | publication en série |
| Lang. | anglais |
| Media | papier; en ligne; numérique |
| Province | Colombie-Britannique |
| SNRC | 92E/15; 92E/16; 92F/04; 92K/06; 92K/07; 104K; 104M; 104N |
| Région | Île de Vancouver; Kennedy Lake; West Redonda Island; Tlupana Arm; Atlin Road; Hurricane Creek |
| Lat/Long OENS | -127.0000 -125.0000 50.2500 48.7500 |
| Lat/Long OENS | -136.0000 -132.0000 60.0000 58.0000 |
| Sujets | gisements minéraux; gîtes minéralogiques; minéralisation; brucite; dérivé; métaux; magnesium; magnésie; minéraux industriels; géologie économique |
| Illustrations | cartes de localisation; photographies; diagrammes; tableaux |
| Résumé | (disponible en anglais seulement)
Brucite is a natural magnesium hydroxide [Mg(OH)2] particularly sought after for its flame-retardant properties, as a raw mineral for the production of caustic
or dead-burned magnesia, a variety of other industrial mineral uses, and as a high-grade ore mineral for the production of magnesium metal. Brucite has an advantage over magnesium carbonates, such as magnesite and dolomite, because it does not
contain CO2 in its crystal structure. Consequently, there is no CO2 released during the calcining or other processing of this mineral except from fuel combustion. This advantage may become even more important in the future as CO2 is considered the
main greenhouse gas contributing to global warming. Carbonate-hosted contact metamorphic/metasomatic (skarn-type) brucite deposits have the best economic potential. The sequence of calcosilicate metamorphic index minerals starting from
unmetamorphosed magnesium-bearing carbonate (dolostone or magnesite-bearing rock) to igneous intrusion contact consists of talc, tremolite, forsterite and brucite/periclase. This sequence can be used to focus exploration efforts. The current
worldwide brucite market is probably less than 100,000 t/y but it is increasing rapidly. High-grade brucite deposits are expected to become hot exploration targets over the next few years. |
| GEOSCAN ID | 285982 |
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