CNR ExploRA

Articolo in rivista, 2023, ENG, 10.3390/fractalfract7110776

Fractal and Spectral Analysis of Seismicity in the Lai Chau Area (Vietnam)

Telesca Luciano, Thai Anh Tuan, Cao Dinh Trong, Cao Dinh Trieu, Dinh Quoc Van, Mai Xuan Bach, Paun Viorel-Puiu

a. Institute of Methodologies for Environmental Analysis, National Research Council, Tito, 85050, Italy b. Institute of Geophysics, Vietnam Academy of Science and Technology, Hanoi, 100000, Viet Nam c. Innovations for Sustainable and Responsible Mining (ISRM) Research Group, Hanoi University of Mining and Geology, Hanoi, 100000, Viet Nam

The time dynamics of the instrumental seismicity recorded in the area of the Lai Chau reservoir (Vietnam) between 2015 and 2021 were analyzed in this study. The Gutenberg-Richter analysis of the frequency-magnitude distribution has revealed that the seismic catalog is complete for events with magnitudes larger or equal to 0.6. The fractal method of the Allan Factor applied to the series of the occurrence times suggests that the seismic series is characterized by time-clustering behavior with rather large degrees of clustering, as indicated by the value of the fractal exponent (Formula presented.). The time-clustering of the time distribution of the earthquakes is also confirmed by a global coefficient of variation value of 1.9 for the interevent times. The application of the correlogram-based periodogram, which is a robust method used to estimate the power spectrum of short series, has revealed three main cycles with a significance level of (Formula presented.) (of 10 months, 1 year, and 2 years) in the monthly variation of the mean water level of the reservoir, and two main periodicities with a significance level of (Formula presented.) (at 6 months and 2 years) in the monthly number of earthquakes. By decomposing the monthly earthquake counts into intrinsic mode functions (IMFs) using the empirical decomposition method (EMD), we identified two IMFs characterized by cycles of 10 months and 2 years, significant at the 1% level, and one cycle of 1 year, significant at the 5% level. The cycles identified in these two IMFs are consistent with those detected in the water level, showing that, in a rigorously statistical manner, the seismic process occurring in the Lai Chau area might be triggered by the loading-unloading operational cycles of the reservoir.

Fractal and fractional 7 (1), pp. Art.n.776-1–Art.n.776-13