Constrained Gravity Inversion for the Moho Depth and Tectonic Patterns in South China Sea

The South China Sea, situated at the convergence of the Tethys and Pacific tectonic domains, holds immense geological significance due to its interaction with multiple tectonic plates(Hall2002; Hayesand Nissen2005; Metcalfe2011). With its abundant sedimentary basins, the region is of paramount importance for geological and structural studies, particularly in relation to its potential for oil and gas resources. In this study, we propose the utilization of satellite gravity data to analyze the tectonic structure of the South China Sea, focusing on three key areas: 1. High-resolution construction of gravity gradient anomalies and fault identification: By integrating Fast Fourier Transform algorithms with satellite gravity anomalies and high-resolution terrain elevation data, we obtaina comprehensive dataset of full tensor gravity gradient information. Through spatial analysis of this data, we successfully identify 17 significant and deep faults, as well as partition the study area into 9 distinct tectonic units characterized by well-defined geological structures. 2. Moho Depth Determination and Interpretation: Employing an improved regularization Bott's method, we determine the Moho depth using information obtained from sonar-buoy detection and submarine seismograph detection profiles. Regularization parameters are introduced to ensure the smoothness of the inversion results. By analyzing the distribution characteristics of the Moho and its relationship with tectonic units, we conduct a comprehensive analysis to comprehend the coupling between shallow and deep structures. The resultsreveal distinct regional characteristics in the depth distribution of the Moho surface in the South China Sea, shedding light on the distribution of continental crust, oceanic crust, and the ocean-continent transition zone. 3. Comprehensive Geophysical Analysis: We employ a combination of seismically constrained Moho undulation, gravity data, gravity gradient anomalies, and unconstrained 3D correlation imaging to investigate the crustal structure of the South China Sea. Integrating various geophysical datasets, we gain a deeper understanding of the distribution of continental crust, oceanic crust, and transitional crust within the region. Notably, the results shows that the trench-island arc-back arc basin systemplays a pivotal role in the active continental margin of the Western Pacific. This comprehensive analysis provides valuable insights into the tectonic dynamics and geological processes occurring in the South China Sea region. *This study was supported by y the Basic Frontier Science Research Program of the ChineseAcademy of Sciences (No. ZDBS-LY-DQC028). Reference: Hall, R. (2002). Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations, J. Asian Earth Sci. 20:353431. Hayes, D.E., Nissen, S.S. (2005). The South China Sea margins: implications for rifting contrasts, Earth Planet Sci. Lett., 237: 601616. Metcalfe, I. (2011). Tectonic framework and phanerozoic evolution of Sundaland, Gondwana Res., 19 (1):321.