J. N. Bubb, Douglas Perry; Porosity in some synthetic dolomites. Journal of Sedimentary Research ; 38 (1): 247–249. doi: https://doi.org/10.1306/74D7194C-2B21-11D7-8648000102C1865D
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Porosity formed during laboratory dolomitization of large calcite crystals is in good agreement with the 13 percent theoretically expected by the idea of local-source dolomitization. The voids formed are irregular in size, shape, and distribution.
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