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myrmekite - traducción al ruso
ROCKY GROWTHS OF QUARTZ
Myrmekitic texture
![Fractured [[alkali feldspar]] filled with central quartz and myrmekite during Ca-metasomatism](https://commons.wikimedia.org/wiki/Special:FilePath/Ca-myrmekite.gif?width=200 "Fractured [[alkali feldspar]] filled with central quartz and myrmekite during Ca-metasomatism")
![Ghost myrmekite in Mount Rubidoux [[leucogranite]]](https://commons.wikimedia.org/wiki/Special:FilePath/Ghost myrmekite.gif?width=200 "Ghost myrmekite in Mount Rubidoux [[leucogranite]]")
![Rim myrmekite on zoned [[plagioclase]] against interstitial [[microcline]] (gray and black)](https://commons.wikimedia.org/wiki/Special:FilePath/Rim myrmekite.gif?width=200 "Rim myrmekite on zoned [[plagioclase]] against interstitial [[microcline]] (gray and black)")
![Wartlike myrmekite in megacrystal [[quartz monzonite]] from Twentynine Palms, California](https://commons.wikimedia.org/wiki/Special:FilePath/Wartlike myrmekite.gif?width=200 "Wartlike myrmekite in megacrystal [[quartz monzonite]] from Twentynine Palms, California")
myrmekite
общая лексика
мирмекит
Wikipedia
Myrmekite
Myrmekite is a vermicular, or wormy, intergrowth of quartz in plagioclase. The intergrowths are microscopic in scale, typically with maximum dimensions less than 1 millimeter. The plagioclase is sodium-rich, usually albite or oligoclase. These quartz-plagioclase intergrowths are associated with and commonly in contact with potassium feldspar. Myrmekite is formed under metasomatic conditions, usually in conjunction with tectonic deformations. It has to be clearly separated from micrographic and granophyric intergrowths, which are magmatic.
