What Is Poikilitic Texture? | Contextresponse. Com
Poikilitic texture refers to crystals, typically phenocrysts, in an igneous rock which contain small grains of other minerals. In igneous rocks Poikilitic texture is widely used to determine order of crystallization; if one mineral is enclosed by another then the enclosed grain must have been the first to crystallize.

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Accordingly, what is Ophitic texture?

Ophitic texture is the association of lath-shaped euhedral crystals of plagioclase, grouped radially or in an irregular mesh, with surrounding or interstitial large anhedral crystals of pyroxene; it is characteristic of the common rock type known as diabase.

what is coarse grained texture? Coarse-Grained (Phaneritic) Textures. Coarse-grained textures generally indicate magmas that slowly cooled deep underground. Slow cooling gives crystals enough time to grow to easily seen sizes (i.e., larger than 1 mm). Thus, you can often figure out the relative order in which the minerals crystallized from the magma.

Accordingly, how do you describe the texture of a rock?

The texture of a rock is the size, shape, and arrangement of the grains (for sedimentary rocks) or crystals (for igneous and metamorphic rocks). Also of importance are the rock's extent of homogeneity (i.e., uniformity of composition throughout) and the degree of isotropy.

What is granular texture?

Definition of granular texture. A rock texture resulting from the aggregation of mineral grains of approx. used to describe an equigranular, holocrystalline igneous rock whose particles range in diameter from 0.05 to 10 mm.

Related Question Answers

What is the texture of gabbro?

Gabbro is mafic, intrusive, coarse-grained rock with allotriomorphic texture. Gabbros contain mainly ferromagnesian minerals and plagioclase, the amount of ferromagnesian minerals equaling or exceeding that of the plagioclase.

What is the texture of pegmatite?

Pegmatitic Textures. A pegmatitic texture is one in which the mineral grains are exceptionally large. This texture is found in intrusive rocks. The extra large size does not mean that they cooled extra slowly. Instead, the large crystals of a pegmatite formed in a magma that was extra rich in dissolved water.
David Miller

David Miller

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