23 Petrology, Mineralogy, and High-Temperature Geochemistry
Tuesday, 19 May 2020
8:00 AM - 12:00 PM
Lake Superior Ballroom L
SPECTRAL FLUORESCENCE OF LIPTINITE MACERALS IN THE LOWER KITTANNING COAL AND OTHER PENNSYLVANIAN-AGE COALS
Paper number: 23-11
Program: Theme Sessions
Time: 11:15 AM – 11:35 AM
Authors
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Sue RimmerSouthern Illinois University, Carbondale, IL
Abstract
Preliminary results show that all three liptinite maceral types show an increase in λmax with sporinite ranging from 567-642 nm, cutinite ranging from 570-662 nm, and resinite ranging from 553-616 nm. Resinite has a higher average relative λmax intensity, and lower λmax wavelength and Q compared to sporinite and cutinite in the Lower Kittanning Coal. Differences in spectral fluorescence properties may be influenced by changes in depositional environment and/or in plant precursors, the stage of development of the precursor materials, and their level of preservation, all of which could result in multiple populations of individual macerals.
Geological Society of America Abstracts with Programs. Vol. 52, No. 5
doi: 10.1130/abs/2020NC-348147
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