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Ophitic texture between an augite (blue-green) oikocryst surrounding smaller plagioclase (black and white) chadacrysts

Poikilitic texture refers to igneous rocks where large later-formed less perfect crystals ('oikocrysts') surround smaller early-formed idiomorphic crystals ('chadacrysts') of other minerals.[1] A poikilitic texture is most easily observed in petrographic thin sections.

In some rocks there seems to be little tendency for the minerals to envelop one another. This is true of many gabbros, aplites and granites. The grains then lie side by side, with the faces of the latter moulded on or adapted to the more perfect crystalline outlines of the earlier.[1]

Ophitic

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A variety of poikilitic texture, known as ophitic texture, is where laths of plagioclase are enclosed in pyroxene, olivine or other minerals. It is very characteristic of many diabases, in which large crystals of augite enclose smaller laths of plagioclase feldspar. Biotite and hornblende frequently enclose feldspar ophitically; less commonly iron oxides and sphene do so. In peridotites the "lustre-mottled" structure arises from pyroxene or hornblende enveloping olivine in the same manner. In these cases no crystallographic relation exists between the two minerals (enclosing and enclosed).[1]

See also

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References

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  1. ^ a b c Wikisource One or more of the preceding sentences incorporates text from a publication now in the public domain: Flett, John Smith (1911). "Petrology". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 21 (11th ed.). Cambridge University Press. p. 330.


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Gabbro

crystal habits. Gabbro is usually equigranular in texture, although it may also show ophitic texture (with laths of plagioclase enclosed in pyroxene).

List of rock textures

Mylonitic Nematoblastic Ocelli Oolitic; see also limestone Ophitic texture Orbicular texture Orthocumulate Panidiomorphic Pegmatitic Peloidal Perthitic

Ophite

characteristic texture of certain dolerites after an occurrence in the Pyrenees Ophitic, a type of poikilitic texture in igneous rocks Ophitic dialect, a

Northwest Africa 16788

porphyritic texture. There are olivine phenocrysts with a maximum size of 3 mm that are embedded into a groundmass of maskelynite and ophitic pyroxene.

Diabase

easily confused with diorite. Diabase normally has a fine but visible texture of euhedral lath-shaped plagioclase crystals (62%) set in a finer matrix

Farmington Gabbro

pyrite, pyrrhotite, and hercynitic spinel. The main texture in the gabbro is ophitic to sub-ophitic, but hornblende and plagioclase are subhedral to anhedral