Mikrolitik porfirik doku, kayaçlarda bulunan küçük, ince taneli kristallerin (mikrolitlerin), fenokristaller olarak adlandırılan daha büyük kristallerin etrafını sardığı bir yapıdır 13.
Bu dokuya sahip kayaçlar, genellikle volkanik magmatik kayaçlar olup, hızlı soğuma sonucu oluşurlar 34.
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