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Pseudomorph
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==Epimorph and incrustation pseudomorph== An '''incrustation pseudomorph''', also called epimorph, results from a process by which a mineral is coated by another and the encased mineral dissolves. The encasing mineral remains, and retains the shape of the original mineral or material. Alternatively, another mineral may fill the space (the mold) previously occupied by some other mineral or material. Examples of quartz epimorph after calcite are found in the La Viesca Mine, Siero (Asturias), Spain.
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