Dolomite, also called dolomite rock, dolostone or dolomitic rock, is a sedimentary carbonate rock containing a high percentage of the mineral dolomite, calcium magnesium carbonate. Most dolomite formed as a magnesium replacement of limestone or lime mud before lithification, a process called dolomitization. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Formation ClassSedimentary carbonate (formed mainly by magnesium replacement of limestone or lime mud before lithification, called dolomitization) 1 Classification
Classification UseBuilding and Construction 2 Connections
Associated With
Dolomitization source: dolomite forms as a magnesium replacement of limestone (or lime mud).
Source Dolomite (Wikipedia)
Classified As
In Discipline
Sources
1. Dolomite (Wikipedia)
Wikimedia FoundationLead section
most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification.
Lead section
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2.
View the Source 2. Geology.com: Dolomite: Mineral and Rock
Geology.comUses of DolomiteQuote, Uses of Dolomite
The most common use for dolostone is in the construction industry.
View the Source Wikidata: Dolomite
Wikidata Q1134814
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