Twelve shale fracture veins and forty-nine fluid inclusion
assemblages
within the veins of 3800–4200 m in three wells located in different
tectonic zones in the Yuxi Region, southern Sichuan Basin were selected
in this study. The burial and thermal histories of single wells were
reconstructed, and time–temperature–pressure of oil
and gas filling were clarified using microscopy observation, Raman
microprobe analyses, geochemical tests, and fluid inclusion microtemperature
measurement. The shale fracture veins of the Wufeng-Longmaxi Formation
in the Yuxi Region are mainly formed vertically and horizontally,
where the vein-forming fluids are derived from endogenous fluids.
A large number of methane inclusions, bituminous inclusions, and methane-bearing
bituminous inclusions within the veins confirm the process of oil
cracking gas and kerogen cracking gas. The homogeneous temperature
(Th) of the aqueous inclusions contemporaneous with the bituminous
inclusions ranges from 109.3 to 174.1 °C, which were trapped
during 220 to 250 Ma. The homogeneous temperature of the aqueous inclusions
contemporaneous with the methane inclusions ranges from 137.3 to 226.8
°C, which were trapped during 160 to 195 Ma and 51 to 56 Ma.
The trapped pressure calculated by high-density methane inclusions
(0.246–0.293 g/cm
3
) is between 82.9 and 140.1 MPa,
with a pressure coefficient between 1.64 and 2.07. The formation pressure
coefficient is nearly two, indicating that the current overpressure
is inherited from the overpressure at the maximum burial depth. The
earlier the fracture vein opening, the less the damage to the shale
gas accumulation, and the more opening-closing phases, the lower the
homogeneous temperature of the gas–liquid two-phase aqueous
inclusions coeval with the high-density methane inclusions and the
greater the degree of damage to the shale gas accumulation. The results
provide a basis for further study on the genesis of overpressure and
the migration of shale gas.