After several years of extensive exploration, a series
of oil and
gas reservoirs or structures have been discovered in the Dongdaohaizi
sag, situated in the hinterland of the Junggar Basin. However, in
recent years, some wells around the sag have failed. Herein, sedimentary
facies, the plane distribution of dark mudstone, geochemical characteristics
of source rocks, and the control of sedimentary facies on the distribution
and development of source rocks in the Permian Pingdiquan Formation
in the Dongdaohaizi sag were systematically investigated. A combined
geological and geochemical method was used to fully understand the
distribution law and resource potential of the source rocks in this
area. Investigation results indicate that the Pingdiquan Formation
primarily inherited continuous deposition, and the sedimentary facies
of the sag, such as semideep lake, shore-shallow lake, prefan delta,
fan delta front, and fan delta plain, were developed from the center
sag to the outside. The fan delta facies, predominantly distributed
in the northern margin of the sag, are characterized by lithology
mainly composed of sandy conglomerate and coarse sandstone. The sandstone
has a coarse particle size and poor sorting ability, while lacustrine
mudstone is widely developed in the sag with a large sedimentary thickness,
which is the primary source rock of the Dongdaohaizi sag. The source
rocks in the Pingdiquan Formation exhibit medium-to-good quality.
The organic matter is categorized as types II1–III,
and the thermal evolution maturity is in the mature-high mature stage,
indicating a high resource potential. The development of the source
rock in the Dongdaohaizi sag is closely related to the sedimentary
environment. The sedimentation rate of fan delta facies is high and
burial is fast, bringing a large amount of terrestrial organic matter
to the lake, thereby increasing the nutrition and organic matter quantity
of the lake. Due to the stable water of the lake, low energy at the
bottom, and medium conditions of strong reduction, a large amount
of organic matter accumulated in the deep to semideep lake facies
of the study area, resulting in the development of thick dark mudstone
with a thickness of over 400 m. The abundance of organic matter has
reached a good level, and the maturity and content of organic matter
are high, signifying a high hydrocarbon-generation potential.