Myrmekite describes 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.
Read more about Myrmekite: Etymology, Myrmekite Formed During K-metasomatism, Myrmekite Formed During Ca-metasomatism, Myrmekite Formed During Na-Ca-metasomatism, Occurrence, Formation