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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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Subject	Predicate	Object	Confidence	Src
Calc–silicate rock	is a	rock produced by metasomatic alteration of existing rocks in which calcium silicate minerals	0.90	text

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