Vitrinite reflectance anisotropy as a tectonic fabric element
- 1 January 1981
- journal article
- Published by Geological Society of America in Geology
- Vol. 9 (4) , 165-168
- https://doi.org/10.1130/0091-7613(1981)9<165:vraaat>2.0.co;2
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).Keywords
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