Dolostone

Dolostone
Triassic dolomitic rocks from Slovakia.
Oberer Hauptdolomit in the Karwendel range, Northern Limestone Alps.

Dolostone or dolomite rock is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite. In old U.S.G.S. publications it was referred to as magnesian limestone. Most dolostone formed as a magnesium replacement of limestone or lime mud prior to lithification.[1] It is resistant to erosion and can either contain bedded layers or be unbedded. It is less soluble than limestone in weakly acidic groundwater, but it can still develop solution features over time.

The term dolostone was introduced to avoid confusion with the mineral dolomite. The usage of the term dolostone is controversial because the name dolomite was first applied to the rock during the late 18th century and thus has technical precedence. The use of the term dolostone is not recommended by the Glossary of Geology published by the American Geological Institute. It is, however, used in some geological publications.

References

  • Blatt, Harvey; Tracy, Robert J. (1996). Petrology; Igneous, Sedimentary, and Metamorphic (2nd ed.). W. H. Freeman. pp. 317–323. ISBN 0-7167-2438-3. 
  • Tucker, M. E.; V. P., Wright (1990). Carbonate Sedimentology. Blackwell Scientific Publications. ISBN 0-632-01472-5. 
  • Zenger, D. H.; Mazzullo, S. J. (1982). Dolomitization. Hutchinson Ross. ISBN 0-87933-416-9. 

Notes

  1. ^ Zenger & Mazzullo, 1982
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