Diorite
Deep igneous rocks made of equal amounts of alkali feldspar and intermediate plagioclase, the most common stained ingredients are amphibole, biotite and pyroxene, and accessory minerals apatite and sfen; volcanic equivalent: tackle. From Wikipedia, the free encyclopedia
Diorite ( /ˈdaɪ.əˌraɪt/) is a melted rock that has cooled made mostly of the silicate minerals (materials made of silicon and oxygen). Diorite is between basalt and granite. Diorite is usually grey to dark-grey in color, but it can also be black or bluish-grey, and often has a greenish cast. It is distinguished from gabbro (basalt) because the material in diorite has more sodium and less calcium. Diorite may have small amounts of quartz, microcline, and olivine. Tiny amounts of muscovite may also be found. If there is a lot of quartz it makes the rock type quartz-diorite (>5% quartz) or tonalite (>20% quartz).
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Diorite has an often speckled texture of coarse grain size.
Diorites may be associated with either granite or basalt intrusions, into which they may merge. Diorite results from the partial melting of a rock above the area where two tectonic plates merge under each other. It is commonly produced in volcanic arcs, and in cordilleran mountain building, such as in the Andes Mountains, as large batholiths. The extrusive volcanic equivalent rock type is andesite.
Occurrence
Diorite is a relatively rare rock. It is found in Leicestershire (one name for microdiorite—markfieldite—exists due to the rock's being found in the village of Markfield) and Aberdeenshire, UK; Guernsey; Sondrio, Italy; Thuringia and Saxony in Germany; Finland; Romania; Northeastern Turkey; central Sweden; the Darrans range of New Zealand;[1] the Andes Mountains.[2]
An orbicular variety found in Corsica is called corsite.
References
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