Resumé
The mineral ilmenite (FeTiO3) is an important component of
heavy-mineral placer deposits and constitutes the largest volume of
valuable mineral in such deposits. The minerals zircon (ZrSiO4) and rutile (TiO2), which occur in lower concentrations than ilmenite in the deposits, have a greater value per ton – c.
1100 and 900 $/ton respectively – compared to ilmenite that ranges from
100 to 200 $/ton depending on its composition. Other minerals such as
staurolite, sillimanite, amphibole and garnet are generally also present
in placer deposits, but are of minor or no commercial value and, e.g.
amphibole needs to be separated from the valuable heavy minerals which
adds to the production cost.
| Originalsprog | Engelsk |
|---|---|
| Sider (fra-til) | 81-84 |
| Antal sider | 4 |
| Tidsskrift | Geological Survey of Denmark and Greenland Bulletin |
| Vol/bind | 33 |
| DOI | |
| Status | Udgivet - 7 jul. 2015 |
Programområde
- Programområde 4: Mineralske råstoffer
Fingeraftryk
Dyk ned i forskningsemnerne om 'Composition of ilmenite and provenance of zircon in northern Brazil'. Sammen danner de et unikt fingeraftryk.Citationsformater
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver