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Matrix dominated rock texture.
The matrix of igneous rocks such as porphyry in which larger crystals phenocrysts are embedded.
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Hot fragments may weld together.
Rocks with porphyritic por fi rit ic texture like this andesite have larger mineral grains or phenocrysts feen o crists in a matrix of smaller grains.
In the dunham classification dunham 1962 system of limestones a mudstone is defined as a mud supported carbonate rock that contains less than 10 grains.
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Andalusite porphyroblasts are up to 2 cm in size and contain chiastolite like inclusions albeit poorly developed.
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Most recently this definition has been clarified as a matrix supported carbonate dominated rock composed of more than 90 carbonate mud 63 μm component.
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A texture wherein plagioclase grains show a preferred orientation due to flowage and the interstices between plagioclase grains are occupied by glass or cryptocrystalline material.
Few small components in a micritic matrix width of picture is 32 mm.
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Matrix dominated by glassy fragments.
Intergrowths of quartz in feldspar.
Most recently this definition has been clarified as a carbonate dominated rock in which the carbonate mud 63 μm component supports a fabric comprising 10 or more very fine sand grade 63 μm or larger grains but where less.
Under the dunham classification dunham 1962 system of limestones a wackestone is defined as a mud supported carbonate rock that contains greater than 10 grains.
In other words they display two distinctive sizes of grains that are visible to the naked eye.
Fine grained minerals enclosed in a larger mineral.
Coarse grained texture slow cooling rate deep in the earth interlocking crystals.
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Has an aphanitic texture.
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Porphyritic rock with a glassy matrix.