The Sichuan Basin in southern China is well-known for
its large
natural gas resource potential stored in Sinian-Cambrian systems.
Recently, high-yield industrial gas flow has been discovered from
the Dengying Formation (Sinian System) and Canglangpu Formation (Cambrian
System) in the Penglai gas area, preluding the multilayer stereoscopic
exploration in Sichuan Basin. However, the origin of the natural gas
and its preserving mechanics is still debated, and thus, in this study
the geochemical characteristics of the natural gas are systematically
analyzed, based on the data from gas composition and hydrocarbon isotope
of a series of local wells. On this basis, the geochemical characteristics
of natural gas in different regions and layers are compared, and the
reasons for these differences from the origin and influencing factors
are analyzed. The results show the following: (1) The natural gas
of the Penglai gas field is dry gas dominated by CH4, and
the Sinian Dengying Formation gas has lower C2H6 content, larger dryness coefficient, heavier δ13C, and lighter δ2HCH4 than the Cambrian
gas, which is associated with the high proportion of hydrocarbons
from the high-maturity Dengying source rocks. (2) The natural gas
from some wells in the lower part of the structure is characterized
by high H2S content and low CH4 content, and
heavy δ13C in the components, which seems to be affected
by the thermochemical sulfate reduction (TSR) effect. (3) The natural
gas from the Penglai gas area has a relatively low maturity, which
appears to be attributed to the continuous sealing ability of the
caprock, which can preserve both the early generated gas and the late
thermal-cracked gas.