Figure 7 - uploaded by Thomas William Bjerstedt
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7-8. Components of banded and non-banded coals. Cannel coal is a non-banded coal that appears waxy. Banded coals contain four main lithotypes: durain (dull, grainy texture, tough), fusain (dull black, charcoal texture, hands get dirty), clarain (bright, satiny texture, brittle), and vitrain (bright, black, glassy, brittle) (from Kentucky Geological Survey, 2006). The historically mined pod of the Cannel Coal near its namesake, Cannel City, is situated on the downthrown side of a large-displacement fault (Irvine-Paint Creek Fault), 15 mi north of this exposure (7-9). The fault shows syndepositional growth because much of the Pikeville and underlying Grundy Formations are unusually thick south of the fault. The Cannel Coal thins and may locally pinch out north of the fault. 

7-8. Components of banded and non-banded coals. Cannel coal is a non-banded coal that appears waxy. Banded coals contain four main lithotypes: durain (dull, grainy texture, tough), fusain (dull black, charcoal texture, hands get dirty), clarain (bright, satiny texture, brittle), and vitrain (bright, black, glassy, brittle) (from Kentucky Geological Survey, 2006). The historically mined pod of the Cannel Coal near its namesake, Cannel City, is situated on the downthrown side of a large-displacement fault (Irvine-Paint Creek Fault), 15 mi north of this exposure (7-9). The fault shows syndepositional growth because much of the Pikeville and underlying Grundy Formations are unusually thick south of the fault. The Cannel Coal thins and may locally pinch out north of the fault. 

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Research
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Suggested citation: Bjerstedt, T.W. 2017. Black shales and deltas, central Appalachians, West Virginia and Kentucky. Unpublished guidebook for site visits by U.S. Dept. of the Interior, Bureau of Ocean Energy Management, Gulf of Mexico Region, New Orleans, LA., June 10-18, 2017. 193 pp. DOI 10.13140/RG.2.2.26292.65923.

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