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  2. Macrocrystalline - Wikipedia

    en.wikipedia.org/wiki/Macrocrystalline

    In geology, macrocrystalline rocks have crystals large enough to easily be identified by sight with the naked eye. Macrocrystalline rocks can be further subdivided into fine-grained, medium-grained, large-grained, and coarse-grained rock, where fine-grained rocks have a grain size of less than 1 mm, medium-grained rocks have a grain size of 1 to 5 mm, large-grained rocks one of 5 to 10 mm, and ...

  3. List of rock types - Wikipedia

    en.wikipedia.org/wiki/List_of_rock_types

    Nephelinite – Igneous rock made up almost entirely of nepheline and clinopyroxene – A silica-undersaturated plutonic rock with >90% nepheline; Norite – Mafic intrusive igneous rock – A hypersthene-bearing gabbro; Obsidian – Naturally occurring volcanic glass; Pegmatite – Igneous rock with very large interlocked crystals

  4. Phenocryst - Wikipedia

    en.wikipedia.org/wiki/Phenocryst

    Some rocks contain both microphenocrysts and megaphenocrysts. [2] In metamorphic rocks, crystals similar to phenocrysts are called porphyroblasts. Phenocrysts are more often found in the lighter (higher silica) igneous rocks such as felsites and andesites, although they occur throughout the igneous spectrum including in the ultramafics.

  5. Porphyroblast - Wikipedia

    en.wikipedia.org/wiki/Porphyroblast

    A similar type of crystal is a phenocryst, a large crystal in an igneous rock. Porphyroblasts are often confused with porphyroclasts, which can also be large outstanding crystals, but which are older than the matrix of the rock [citation needed].

  6. Pegmatite - Wikipedia

    en.wikipedia.org/wiki/Pegmatite

    Large crystals are favored. In normal igneous rocks, coarse texture is a result of slow cooling deep underground. [14] It is not clear if pegmatite forms by slow or rapid cooling. [15] In some studies, crystals in pegmatitic conditions have been recorded to grow at a rate ranging from 1 m to 10 m per day. [16]

  7. Igneous textures - Wikipedia

    en.wikipedia.org/wiki/Igneous_textures

    Phaneritic (phaner = visible) textures are typical of intrusive igneous rocks, these rocks crystallized slowly below Earth's surface. As magma cools slowly the minerals have time to grow and form large crystals. The minerals in a phaneritic igneous rock are sufficiently large to see each individual crystal with the naked eye.

  8. Porphyritic - Wikipedia

    en.wikipedia.org/wiki/Porphyritic

    The large grain in the middle is of a much different size class than the small needle-like crystals around it. Scale box in millimeters. Porphyritic is an adjective used in geology to describe igneous rocks with a distinct difference in the size of mineral crystals, with the larger crystals known as phenocrysts.

  9. Chrysoberyl - Wikipedia

    en.wikipedia.org/wiki/Chrysoberyl

    The resulting rock is igneous in appearance but formed at a low temperature from a water-rich melt, with large crystals of the common minerals such as quartz and feldspar, but also with elevated concentrations of rare elements such as beryllium, lithium, or niobium, often forming their own minerals; this is called a pegmatite. The high water ...

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