Source: Food and Agriculture Organization of the The United Nations
| Deposit Type | Igneous Carbonatite | Igneous Massif-Type Anorthosite | Sedimentary |
|---|---|---|---|
| Host Rock | Carbonatite | Massif-Type Anorthosite | Upwelling-Related Sedimentary Rocks |
| Distribution | 4% of global deposits | 1% of global deposits | 95% of global deposits |
| Shape Of Ore Bodies | Veins and Lenses | Sheets and Lenses | Bedded (stratiform) |
| Rare of Earth Elements | High | Low | Variable |
| Deleterious Trace Elements | Low | Low | High |
| Organic Matter | None | None | High |
| Phosphate Mineralogy | Apatite | Apatite | Carbonate Fluorapatite |
| Associated Minerals | Calcite, Dolomite, Magnetite | Pyroxene, Plagioclase, Ilmenite, Magnetite | Quartz, Clay Minerals, Calcite, Dolomite |
| P2O5 Content | ~5 to 15 wt% | ~5 to 15 wt% | ~8 to 35 wt% |
| Source | Mantle > 50 km depth) | Mantle/Crust (~ 30 to 50 km depth) | Upwelling-related organic matter |
| Mineralization Processes | High temperature crystallization in magma | High temperature crystallization and gravitational settling in magma | Phosphate precipitation in accumulating sediment |
Source: Dr. Sandeep Banerjee, Postdoctoral Fellow/ Researcher Queen's University
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