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Calc–silicate rock

A calc–silicate rock is a rock produced by metasomatic alteration of existing rocks in which calcium silicate minerals, such as diopside and wollastonite, are produced. Calc–silicate skarn or hornfels occur within impure limestone or dolomite strata adjacent to an intruding igneous rock.

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Calc–silicate rock

Nodes12
Edges11
Triples1
Avg. degree1.83
Density0.166667
Components1

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Calc–silicate rock

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Calc–silicate rock → rock produced by metasomatic alteration of existing rocks in which calcium silicate minerals

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Important terminology

calc silicate rock diopside wollastonite skarn hornfels limestone dolomite strata produced metasomatic alteration existing rocks calcium minerals occur within impure

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SubjectPredicateObjectConfidenceSrc
Calc–silicate rockis arock produced by metasomatic alteration of existing rocks in which calcium silicate minerals0.90text

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