Research Article

Origin and Role of Kaolinization in Roll-Front Uranium Deposits and Its Response to Ore-Forming Fluids in the Yili Basin, China

Table 3

Gas hydrocarbon composition in host rocks within the Mengqiguer uranium deposit.

SamplesDistance from underlying coal seam (m)RocksC1
(μl/kg)
C2
(μl/kg)
C3
(μl/kg)
nC4
(μl/kg)
iC4
(μl/kg)
nC5
(μl/kg)
iC5
(μl/kg)
C1/C1/∑C

P-112Coarse-grained sandstone910.2035.3410.720.783.630.371.0017.560.95
P-213Coarse-grained sandstone908.4030.3415.560.831.050.230.7618.630.95
P-321Conglomerate675.2118.6110.010.331.560.170.4421.700.96
P-429Medium-grained sandstone364.3312.815.520.462.110.290.6516.680.94
P-535Sandy conglomerate200.309.814.700.391.560.190.4511.710.92
P-644Fine-grained sandstone194.326.824.100.371.410.200.4414.570.94
P-749Medium-grained sandstone88.802.511.010.090.34<0.050.0921.980.96

C1, methane; C2, ethane; C3, propane; nC4, n-butane; iC4, isobutene; nC5, n-pentane; iC5, isopentane; = C2 + C3 + nC4 + iC4 + nC5 + iC5; ∑C = C1 + C2 + C3 + nC4 + iC4 + nC5 + iC5.