Aluminoceladonite is a low-temperature potassium dioctahedral mica mineral which is an end-member in the illite-aluminoceladonite solid solution series. The chemical formula for aluminoceladonite is K(Mg,Fe2+)Al(Si4O10)(OH)2.[4]
Occurrence
Aluminoceladonite is often referred to as a rare mineral, though its actual abundance may be underestimated due to difficulty of identification. Aluminoceladonite, along with other phyllosilicate minerals in the illite-aluminoceladonite solid solution series, has been observed mainly among finely dispersed, mostly inter-layer-deficient, aluminium-rich potassium-dioctahedral mica varieties occurring in sedimentary rocks.[5]
^Drits, Victor A.; Zviagina, Bella. B; McCarty, Douglas K; Salyn, Alfred L. (2010). "Factors responsible for crystal-chemical variations in the solid solutions from illite to aluminoceladonite and from glauconite to celadonite". American Mineralogist. 95 (2–3): 348–361. Bibcode:2010AmMin..95..348D. doi:10.2138/am.2010.3300. S2CID62881038.
^Zviagina, Bella B.; Drits, Victor A; Środoń, Jan; McCarty, Douglas K.; Dorzhieva, Olga V. (2015). "The illite–aluminoceladonite series: distinguishing features and identification criteria from x-ray diffraction and infrared spectroscopy data". Clays and Clay Minerals. 63 (5): 378–394. Bibcode:2015CCM....63..378Z. doi:10.1346/ccmn.2015.0630504. S2CID100485107.