The Lower Jurassic
reservoir has recently made a significant breakthrough
in petroleum exploration in the Tugerming area of the eastern Kuqa
depression, Tarim Basin, northwest China. Therefore, it is significantly
essential to simulate the hydrocarbon charging process and analyze
the accumulation mechanism in the study area. In our study, we mainly
combine three geochemical techniques to identify the origin of crude
oils and fluid inclusion characteristics in the target well (Tudong
2), including gas chromatography–mass spectrometry (GC–MS),
comprehensive two-dimensional GC-time-of-flight MS (GC × GC–TOFMS),
fluid inclusion analysis, and quantitative fluorescence technique.
Combined comprehensive experiments with a set of burial history and
tectonic thermal evolution history realize the reconstruction of the
hydrocarbon charging process in the Yangxia formation. The results
show that Jurassic coal-bearing source rocks are primary hydrocarbon
sources, and there are three hydrocarbon charging events in the Lower
Jurassic reservoir. First, the mature oils have expelled into the
reservoir during the early-middle period (15–10 Ma) of the
Miocene Kangcun Formation, forming yellow fluorescent oil inclusions
and most of the quantitative grain fluorescence (QGF) indexes exceed
4. Second, numerous condensate oils have charged into the reservoir
in the period of late Miocene Kangcun Formation-early Kuqa Formation
(9–6 Ma), accompanied by blue-white oil inclusions and QGF
on extract intensity greater than 4. Finally, vast natural gas has
accumulated in the reservoir since Kuqa Formation (5–0 Ma),
resulting in the adjustment of ancient reservoir and residual bitumen.
Interestingly, we find that the hydrocarbon accumulation mechanism
is characterized by self-generation and self-storage in the Jurassic
Yangxia Formation, and the study area has prominent characteristics
of late accumulation. Thus, the evidence obtained from our analysis
suggests favorable geological conditions for the formation of a large
oil and gas reservoir in the eastern Kuqa Depression.