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Illite crystallinity information


Figure 1: Illite crystallinity classification chart showing the different metamorphic zones and facies corresponding to IC, adapted from Verdel 2012
Figure 2: Illite structure

Illite crystallinity is a technique used to classify low-grade metamorphic activity in pelitic rocks.[1] Determining the "illite crystallinity index" allows geologists to designate what metamorphic facies and metamorphic zone the rock was formed in and to infer what temperature the rock was formed. Several crystallinity indices have been proposed in recent years, but currently the Kübler index is being used due to its reproducibility and simplicity.[2] The Kübler index is experimentally determined by measuring the full width at half maximum for the X-ray diffraction reflection peak along the (001) crystallographic axis of the rock sample.[3] This value is an indirect measurement of the thickness of illite/muscovite packets which denote a change in metamorphic grade. The method can be used throughout the field of geology in areas such as the petroleum industry, plate tectonics.

  1. ^ Verdel, Charles; Niemi, Nathan; van der Pluijm, Ben A. (2011). "Variations in the Illite to Muscovite Transition Related to Metamorphic Conditions and Detrital Muscovite Content: Insight from the Paleozoic Passive Margin of the Southwestern United States" (PDF). The Journal of Geology. 119 (4): 419–437. Bibcode:2011JG....119..419V. doi:10.1086/660086. S2CID 129686326. Retrieved 7 October 2013.
  2. ^ Cite error: The named reference Abad was invoked but never defined (see the help page).
  3. ^ Eberl, D. D.; Velde, B. (December 1989). "Beyond the Kübler index" (PDF). Clay Minerals. 24 (4): 571–577. Bibcode:1989ClMin..24..571E. doi:10.1180/claymin.1989.024.4.01.

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Illite crystallinity

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spectroradiometry. Illite, for instance, is commonly observed in the vicinity of hydrothermal ore bodies. Higher concentrations of illite may indicate areas...

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evidence of alteration is bleaching, change in colour or change in the crystallinity of micaceous minerals. In such cases, characterising alteration often...

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to calcium-rich clay (montmorillonite) rather than potassium-rich clay (illite). Further weathering, particularly in tropical climates, converts the montmorillonite...

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