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A perthitic texture is an intimate intergrowth of sodic and potassic feldspar resulting from subsolidus exsolution (unmixing of two minerals). Strictly speaking a perthite has blebs or irregular lamellae of sodic feldspar within potassic alkali feldspar, however, the term perthite is often used to describe all types of exsolution in the feldspars. An antiperthite is an intergrowth arising due to exsolution where potassic feldspar is present as blebs or lamellae within a sodic feldspar. The term mesoperthite is used when sodic and potassic feldspars are in broadly equal anbundance. Perthite that can only be observed with the aid of a microscope is known as microperthite. Perthite in which the lamellae are barely visible under a microscope is termed cryptoperthite.

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Perthitic texture is a type of intergrowth of two minerals, typically feldspar minerals, with one appearing as thin, parallel plates or lamellae within the other. It is formed during slow cooling of a rock and is commonly observed in igneous rocks such as granites. This texture is often seen in alkali feldspars, where exsolved lamellae of sodium-rich feldspar (such as albite) occur within a host potassium-rich feldspar (such as orthoclase).

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Q: What is perthitic texture?
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