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The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.



mineral formations whose external form does not correspond to their composition and internal structure. When defining pseudomorphs, the name of the original substance is given, as well as the name of the mineral that has replaced it, while preserving the original shape (for example, a pseudomorph of limonite after pyrite or of chalcedony after wood). In some cases pseudomorphs are given their own names, for instance, the pseudomorph of magnetite after hematite is called mouchketovite.

A distinction is made between simple pseudomorphs, in which one mineral crystallizes in place of another, and complex pseudomorphs, formed by an aggregate of several minerals, such as the aggregates of albite and muscovite in spodumene crystals.

Depending on their origin, pseudomorphs are divided into alteration, substitution, filling, encrustation, and negative pseudomorphs. In pseudomorphs of alteration, there is a chemical bond between the new mineral and the one from which the pseudomorph emerged. Examples include pseudomorphs of limonite after siderite, malachite after azurite, and anglesite after cerussite. A particular type of alteration pseudomorph is the paramorph, which has the same composition as the original crystal but a different crystalline structure. Such a change is usually observed in polymorphic transitions (paramorphs of pyrite after marcasite, calcite after aragonite, and sphalerite after wurtzite).

Substitution pseudomorphs are created during various metasomatic processes and are characterized by a lack of apparent relationship between the chemical composition of the newly formed minerals and the preexisting ones, for example, pseudomorphs of quartz after barite or of magnetite after asbestos and all pseudomorphs in organic remains. Filling pseudomorphs occur when the bulk of the material in a body is dissolved out, and the remaining cavity, with a shape characteristic of the body, is later filled by another mineral (pseudomorphs of sandstone after halite).

In the case of encrustation pseudomorphs, one mineral entirely covers and surrounds the crystals of another in the form of crusts (chalcopyrite crusts on magnetite or quartz crusts on fluorite). Negative pseudomorphs are imprints of the crystal of one mineral on the other or cavities from the dissolving of preexisting mineral grains.

The study of pseudomorphs is very important for clarifying the principles of change in minerals and for establishing preexisting conditions and the nature of chemical reactions during the formation of deposits of useful minerals.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
References in periodicals archive ?
At places the complete transformation of hornblende to chlorite is visible in the form of pseudomorph left after hornblende.
Braunite occurs in good crystals in the manganese deposit at Ohrenstock near Ilmenau, in the Thuringian Forest about 100 km south of Ilfeld, but in the Ilfeld manganese veins it did not form good macrospecimens--lustrous crystals to 5 mm have been noted rarely, and braunite pseudomorphs after manganite occasionally have appeared (, 2010).
However, subsoils formed in saprolite may contain fragile pseudomorphs of primary minerals resulting in minor fabric alteration by ripping.
Ink Release is observed in several forms: (a) a cloud (n = 25), either diffuse or of interconnecting ink blobs, (b) a single pseudomorph (n = 9) or two or more consecutive pseudomorphs (n = 2) that hold their shape, (c) a diffuse puff (n = 6), (d) a long slender rope (n = 2), (e) a short, thin string (n = 2), and (f) alternating with defecation (n = 1).
The role of capillary forces acting as hydrostatic tension in capillary water during the dissolution and initial crystallization in the clay pseudomorphs is not yet known.
The Eel Bed of the Kokomo Limestone contains sedimentary structures that include bird's-eye (fenestrate) structures, algal mats, gypsum/anhydrite blebs and pseudomorphs, penecontemporaneous dolomite, and intraformational storm tide deposits, that we interpret as indicative of a supratidal (Shinn 1983; Hardie & Shinn 1986) depositional environment.
Baculi can be regarded as original structures (our preferred interpretation) or as pseudomorphs formed during the earliest stages of fossilization (e.g.
The presence of platy goethite pseudomorphs and platy leach casts after pyrrhotite provide important evidence for the origin of Okorusu fluorite orebodies by the replacement of pegmatitic carbonatite.