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Carbonate Intraclasts, Mt. Yamnuska
Carbonate Intraclasts, Mt. Yamnuska
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Carbonate Intraclasts, Mt. Yamnuska
Carbonate intraclasts are carbonate fragments that have been transported by tides, waves and storms. The internal structure of each clasts can still be seen but they have been rearranged and deposited together. The allochems in this sample are composed of micrite (carbonate mud) and deposited in spary calcite. Allochems are the recognizable grains present in carbonate rocks
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Date
07/30/2016
Creator
Dolphin, Glenn
Digital Publisher
Calgary : University of Calgary
Location
Country
Canada
Municipality
Kananaskis Improvement District
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Permitted uses are outlined in License and Usage Rights. Usage Restrictions can only be waived by the copyright holder. Add to cart and make a request if you have any questions.
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In Copyright
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Conditions of Use
https://libanswers.ucalgary.ca/faq/199047
License URL
https://creativecommons.org/licenses/by/4.0/
License
CC BY 4.0
Attribution
Attribution
Carbonate Intraclasts, Mt. Yamnuska, 2016, (CU123293) by Dolphin, Glenn, is used under CC BY 4.0. Courtesy of Geoscience Images Collection, Libraries and Cultural Resources Digital Collections, University of Calgary.