Petrukite is a relatively uncommon mineral that belongs to the chlorite group. It has a chemical formula of (K, Na)2Fe2+5Al(Si7Al)O22(OH)2 and appears as small, greenish-black aggregates. The spelling of "petrukite" can be explained using the International Phonetic Alphabet (IPA) transcription, which is /pɛtˈrukaɪt/. It is pronounced as "pet-roo-kite" with an emphasis on the first syllable. Petrukite was discovered in 1969 in the Kola Peninsula, Russia, and was named after the Russian mineralogist Petr Petrovich Petruk.
Petrukite is a mineral that belongs to the silicate group, specifically to the phyllosilicates subgroup. It is a rare mineral that occurs as green, transparent to translucent platy crystals or thin flakes. The name "petrukite" is derived from its type locality at the Petruk's Group iron mine in the Kovdor complex, Russia.
The chemical formula of petrukite is typically given as A2M3Si4O10(OH)2, where A represents monovalent cations like sodium or potassium, and M represents divalent cations such as magnesium or iron. The crystal structure of petrukite consists of sheets of interconnected SiO4 and Si2O7 tetrahedra, with hydroxyl groups connecting the sheets.
Petrukite has a Mohs hardness of approximately 2.5, making it a relatively soft mineral. It is known for its distinctive olive-green color, which can vary in intensity depending on the presence of impurities. The mineral has a vitreous to pearly luster and is characterized by its perfect cleavage, which allows it to be easily split into thin layers.
Although petrukite is not widely utilized commercially, it holds significance in the field of mineralogy and geology due to its rarity and unique crystal structure. Its occurrence is primarily associated with metamorphic rocks and hydrothermal veins. Researchers and collectors value petrukite for its aesthetic beauty and as a subject of scientific study to enhance our understanding of Earth's mineral diversity and geological processes.