Chlorite-illite tonstein in high-rank coals from Queensland, Australia; notes on regional epigenetic grade and coal rank

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ID: 301131
1966
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Abstract
Crystals of dioctahedral illite and chlorite occur in tonsteins associated with upper Permian coals of semi-anthracite rank in the Bowen basin, Queensland, whereas kaolinite is absent. It is inferred that the chlorite and illite were formed by replacement of kaolinite. Some minor illite (2M), twinned albite, and chlorite of detrital origin are also present. The chlorite-dioctahedral illite assemblage is related to the rank of the associated coals. Persistence of kaolinite in tonsteins of other high-rank coals is ascribed to compositional factors.
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openalex_W1968791664 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Hanan J. Kisch
Journal american journal of science
Year 1966
DOI
10.2475/ajs.264.5.386
URL
https://ajsonline.org/article/59137.pdf
Keywords Keywords not found

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