Along-Strike Variation in the Shallow Velocity Structure beneath the Chenghai Fault Zone, Yunnan, China, Constrained from Methane Sources and Dense Arrays

Abstract

Abstract The fine structure of the fault zone and the surrounding area is the basis for understanding the process of earthquake nucleation and rupture propagation. To obtain the high-resolution structure of the Chenghai fault (CHF) and the nearby basins, we deployed two dense arrays and excited eight methane sources across the fault from October to November 2020. Based on the 611 P-wave travel times, we obtained the shallow velocity structure beneath the arrays using the simul2000 travel-time inversion program, and the results are as follows: (1) the shallow velocity structure beneath the CHF is very complex, with obvious velocity contrasts on both the sides of the regional fault; (2) low-velocity zones (LVZs) beneath the CHF show clear along-strike variations. The LVZs extend to ∼500 m in depth with widths of ∼2 km and ∼5 km beneath the Qina and Pianjiao arrays, respectively, which are consistent with the Quaternary sediments, and the velocity contrasts along the interface of the LVZ can reach 20%–50%; and (3) the distribution of shallow surface tectonic geomorphology is mainly controlled by regional fault activities that are formed under the combined action of regional near-east–west stretching and clockwise rotation of microblocks. Our results can help improve cognition and seismic hazard assessment for potential earthquakes on the CHF, as well as lay the foundation for understanding the seismic wave velocity variation mechanism in the fault zone.