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Skarns or tactites are coarse-grained metamorphic rocks that form by replacement of carbonate-bearing rocks during regional or contact metamorphism and metasomatism. Skarns may form by metamorphic recrystallization of impure carbonate protoliths, bimetasomatic reaction of different lithologies, and infiltration metasomatism by magmatic-hydrothermal…
Regions, Petrology & Classification
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skarns protolith form rocks fluids deposits metasomatism metamorphism minerals iron limestone contact composition associated hornfels ore variety metamorphic hydrothermal carbonate
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| tin | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| tungsten | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| manganese | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| copper | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| gold | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| zinc | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| lead | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| nickel | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| molybdenum | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| iron.A skarn is formed by a variety of metasomatic processes during metamorphism between two adjacent lithologic units | instance of | Skarn deposits are economically valuable as sources of metals | 0.80 | text |
| shale | instance of | Skarns can form in almost any rock type | 0.80 | text |
| granite | instance of | Skarns can form in almost any rock type | 0.80 | text |
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