| Citation: | GONG Fangjing，YE Qing，QIN Jun，et al. Control of NW-trending basement faults on Cenozoic basin evolution in Lishui East Sag, East China Sea Basin[J]. Bulletin of Geological Science and Technology，2026，45（3）：180-194 doi: 10.19509/j.cnki.dzkq.tb20250366
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NW-trending structures are the dominant factor controlling the "north–south segmentation" of rift architecture in the East China Sea Basin, yet studies on their specific control mechanisms of basin evolution remain poorly constrained. To investigate this issue, the study uses the Lishui East Sag as a case study.
Based on newly acquired
The results revealed four NW-trending dextral transfer zones (TZ1–TZ4) in the basement of the Lishui East Sag, which exhibited varying degrees of activity during both the rifting stage and the post-rifting stage. ① During the rifting stage, the NW-trending transfer zones accommodated variations in rift architecture along strike, causing NE-trending faults to branch, distort, or reorient into NW-trending faults. This process segmented NE-trending structural units and led to a structural pattern characterized by "east–west zonation and north–south segmentation." During the rifting episode I (sedimentary period of the Yueguifeng Formation), NW-trending basement faults in TZ1-TZ4 were all active, defining or partially defining sub-sag boundaries. During the rifting episode II (sedimentary period of the Lingfeng Formation), TZ2 and TZ3 remained active, while TZ1 and TZ4 activity greatly weakened. In addition, active segments along NW-trending transfer zones migrated southeastward. ② During the post-rifting stage, NW-trending basement faults continued to influence fault development. Extensional faults were more developed within the NW-trending transfer zones, and reoriented to an EW strike, forming right-stepping en echelon patterns. Additionally, NW-trending basement faults controlled the development of NW-trending valley systems on the eastern Yandang uplift in the eastern part of the sag and served as preferential pathways for volcanic conduits in the post-rifting stage. ③ Integrating seismic data and previous studies, this study proposed that the NW-trending basement faults in the Lishui East Sag originated from the NW-trending thrust fault system formed during the Mesozoic Indosinian orogeny.
In summary, NW-trending basement faults play a crucial role throughout the Cenozoic evolution of the Lishui East Sag, governing its rift architecture, fault systems, magmatic activity, and sediment source pathways. This study provides significant insights into the tectonic evolution of the East China Sea Basin and enhances understanding of how pre-existing basement faults control rift basin development.
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