Abstract
The anisotropy of the coal maceral vitrinite was analyzed in relation to the tectonic setting of a coal from the Southern Anthracite Field in Pennsylvania. For the coal studied, the maximum-intermediate reflectance plane essentially paralleled the axial plane of the synclinorium (N66°E strike, 64°SE dip).
| Original language | English |
|---|---|
| Pages (from-to) | 165-168 |
| Number of pages | 4 |
| Journal | Geology |
| Volume | 9 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1981 |
ASJC Scopus subject areas
- Geology
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