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EarthWord: Dedolomitization

September 21, 2015

The process in which magnesium is removed from the mineral dolomite (calcium magnesium carbonate) leaving behind the minerals calcite (calcium carbonate) and periclase (magnesium oxide.)

EarthWords is an on-going series in which we shed some light on the complicated, often difficult-to-pronounce language of science. Think of us as your terminology tour-guides, and meet us back here every week for a new word!

An image of calcite.
An image of calcite. Credit: Rob Lavinsky, iRocks.com – CC-BY-SA-3.0 [CC BY-SA 3.0 (http://creativecommons.org/licenses/by-sa/3.0)], via Wikimedia Commons

Definition:

  • The process in which magnesium is removed from the mineral dolomite (calcium magnesium carbonate) leaving behind the minerals calcite (calcium carbonate) and periclase (magnesium oxide.)

Etymology:

  • Dolomite gets its name from the French scientist who discovered it, Déodat de Dolomieu.

Use/Significance in the Earth Science Community:

  • Dedolomitization results from moderate increases in temperature and pressure during various geologic processes. Some of the new minerals formed by the magnesium include oxides, hydroxides, and silicates. The term “dolomitization” refers to the opposite process, where calcite is converted to dolomite by the addition of magnesium.

USGS Use:

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