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Solution breccias

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Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Solution breccias are common and widespread in the geological record. Brecciation may occur entirely within one soluble rock (usually limestone or dolostone) or where more soluble evaporites are removed in mixed evaporite–carbonate and evaporite–redbed sequences. It may be extended upward by mechanical failure (stoping) into overlying insoluble strata, e.g., dissolution of ∼180 m of salt has propagated through 400 m of carbonates overlain by ∼650 m of clays, mudstones, and sandstones at a site in Saskatchewan (Christiansen and Sauer, 2001).

Figure S35
figure 35

A dolomite and dedolomite solution breccia created by preferential dissolution of gypsum in a sabkha sequence, the Bear Rock Formation (Lower–Middle Devonian) at Bear Rock near Fort Norman, Northwest Territories, Canada. The section is ∼15 m in height.

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Bibliography

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© 1978 Dowden, Hutchinson & Ross, Inc.

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Ford, D. (1978). Solution breccias. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_217

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  • DOI: https://doi.org/10.1007/978-1-4020-3609-5_217

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