Abstract
The Springfield (Western Kentucky No. 9) coal of the Carbondale Formation (Middle Pennsylvanian) in the Western Kentucky Coal Field of the Illinois Basin was sampled in eleven mines from one to three channels of three equal benches. The rank of the coal is high-volatile C bituminous in the Moorman Syncline and in the Henderson Basin and high-volatile B bituminous in the Webster Syncline. The percentage of total vitrinite macerals and of total vitrinite plus liptinite was found to decrease significantly from the bottom bench through to the top bench. In a comparison of the sources of variation within the set of maceral data it was found that the only significant variation in the vitrinite and vitrinite plus liptinite percentages was between the benches. Both the rank of the coal and the maceral percentages are varying in a predictable manner.
| Original language | English |
|---|---|
| Pages (from-to) | 17-30 |
| Number of pages | 14 |
| Journal | International Journal of Coal Geology |
| Volume | 2 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jun 1982 |
ASJC Scopus subject areas
- Fuel Technology
- Geology
- Economic Geology
- Stratigraphy