Ammonian illite (NH
4
-illite)-rich late Permian coals
of high rank were discovered in southwestern China. This research
reports new mineralogical and geochemical data of 11 bench samples
from the adjacent Xingying mine, northeastern Chongqing Coalfield,
southwestern China, with an emphasis on the modes of occurrence and
origin of NH
4
-illite. The Xingying coals, with low ash
yields and medium sulfur, have a high rank (semianthrite,
R
o,ran
= 3.67%), owing to the plutonic metamorphism.
Minerals in the coal consist of NH
4
-illite and pyrite and,
to a lesser extent, jarosite, albite, and anatase, with traces of
chamosite, quartz, bassanite, apatite, fluorapatite, florencite, and
rhabdophane. Compared with world hard coals, vanadium is significantly
enriched with a concentration coefficient (CC) higher than 10; Mo
and Pb are enriched (5 < CC < 10); F, Co, Ni, Cu, Ge, Se, Y,
Zr, Nb, Ag, Cd, In, Sn, Cs, Sm, Eu, Tb, Dy, Er, Yb, Hf, Bi, and U
are slightly enriched (2 < CC < 5) in the Xingying coals. Fluorine
in host rocks, including roof, floor, and parting, is significantly
enriched. Fluorine concentration in the coal may be increased greatly
if the coal is mixed with host rocks during mining activity. Hence,
the Xingying coals should be subjected to beneficiation before utilization
for the environment and human health. The Al
2
O
3
/TiO
2
and Eu anomalies demonstrated that the terrigenous
materials come from the mafic basalts of the Kangdian Upland. NH
4
-illite is formed by interaction of pre-existing kaolinite
or K-illite with NH
4
+
released from organic
matter under high temperatures during the process of hydrothermal
alteration. The authigenic chamosite, albite, quartz, anatase, apatite,
fluorapatite, and rhabdophane are also deposited from the hydrothermal
solutions. In addition, the Xingying coals are subjected to marine
influences. Based on the preliminary evaluation, the Xingying coals
cannot be a potential source for critical elements such as rare earth
elements and yttrium. This indicates that not all the late Permian
coals in southwestern China have economic significance for critical
elements.