It
has been controversial whether tectonic stress affects the chemical
structure of coals. To further understand if and how tectonic stress
affects the chemical structure of coals, an investigation into the
macromolecular-level deformation mechanism is quite necessary. Therefore,
we performed deformation experiments on anthracite with axial load
both parallel and perpendicular to the bedding plane. Macromolecular
structure variations during deformation were revealed by a combination
of Raman spectroscopy and high-resolution transmission electron microscopy.
Results show that (1) coal deformation behaviors (brittle deformation
or ductile deformation) are influenced by stress direction, in addition
to the temperature and strain rate, and (2) ductile deformation is
related to the growth of defects, which is more favorable under stress
parallel to the bedding plane, at higher temperature and lower strain
rate, while brittle deformation is presumably due to the direct bond
breakage beyond the elastic limit. On the basis of the study of coal
deformation mechanisms, we suggest that hydrocarbon generation under
stress is possible and that it may become a supplement for the traditional
hydrocarbon generation theory.