Fault characteristics and control on hydrocarbon accumulation of middle-shallow layers in the slope zone of Mahu sag, Junggar Basin, NW China
Yongbo CHEN1,*(
),Xiaogan CHENG2,Han ZHANG1,Chunyang LI2,Yongping MA1,Guodong WANG1
),Xiaogan CHENG2,Han ZHANG1,Chunyang LI2,Yongping MA1,Guodong WANG1
.
Fig. 2.. Section features of faults in slope zone of the Mahu sag (the locations of the sections are shown in Figs. 1 and 3). Cz—Cenozoic; K2a—Cretaceous Ailikehu Fm.; K1tg—Cretaceous Tugulu Group; J3q—Jurassic Qigu Fm.; J2t—Jurassic Toutunhe Fm.; J2x—Jurassic Xishanyao Fm.; J1s—Jurassic Sangonghe Fm.; J1b—Jurassic Badaowan Fm.; T3b—Triassic Baijiantan Fm.; T2k—Triassic Karamay Fm.; T1b—Triassic Baikouquan Fm.; P2w—Permian Urho Fm.; P2x—Permian Xiazijie Fm.; P1f—Permian Fengcheng Fm.; P1j—Permian Jiamuhe Fm.; C—Carboniferous.
