The dynamic metamorphism of tectonically deformed coals
(TDCs)
is closely correlated with the occurrence of coalbed methane. Here,
a Raman detection technique was used to characterize two primary coals
and 14 TDCs sampled from the Huaibei coalfield, allowing for profound
insight into the dynamic metamorphism caused by tectonic stress in
coals. A nine-peak curve fitting method was applied to deconvolute
the first-order Raman spectra, and six structural parameters were
used to characterize the hierarchical evolution of TDC molecules.
The lower A
S/A
Total and A
S/A
D ratios in TDCs indicate that the cross-links in secondary and aggregated
(outer) structures are cleaved by tectonic stress. Once the aromatic
structures are released through the cleavage of cross-links, the outer
structures can be rearranged into a more ordered configuration, as
indicated by the higher I
G/I
A2 ratio in TDCs. Additionally, the basic structural units
(including aromatic structures and side chains) in TDC are also altered
by stress. The increasing values of A
D/A
G and A
(D+A1+A2)/A
Ds illustrate that the size of aromatic
structures and the ratio of small aromatic structures both increase
with increasing coal deformation intensity. The value of A
C/A
Total decreases with increasing
deformation intensity, indicating that oxygen functional groups are
disassociated by tectonic stress. However, as the basic structural
units are commonly rigid and cannot be altered as readily as the outer
structures, the evolution of basic structural units is not always
obvious in weakly deformed coals (such as cataclastic, mortar, and
schistose types) but is more significant in strongly deformed coals
(such as granulitic, scaly, and wrinkle types).