The illite-aluminoceladonite series; distinguishing features and identification criteria from X-ray diffraction and infrared spectroscopy data
Al-rich K-dioctahedral 1M and 1Md micas are abundant in sedimentary rocks and form a continuous compositional series from (Mg,Fe)-poor illite to aluminoceladonite through Mg-rich illite. The complexity and heterogeneity of chemical composition and structural features, as well as the lack of reliable...
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Veröffentlicht in: | Clays and clay minerals 2015-10, Vol.63 (5), p.378-394 |
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