Crustal extension and magmatism along the northeastern margin of the South China Sea: Further insights from shear waves

The northern continental margin of the South China Sea (SCS) is a unique rifted margin that experienced weak magmatism in the syn-rift stage and intense magmatism in the post-rift stage. This area also exhibits a complicated relationship between crustal extension and magmatism. We present the tomographic inversion of seismic P-wave and S-wave velocity models, as well as the Vp/Vs ratio model, in order to delineate the crustal extension and post-rift magmatic features. The velocity structure is created by forward modelling (Raylnvr) and travel-time tomographic inversion (Tomo2D). The results suggest that Mesozoic strata near the Dongsha area has a maximum thickness of similar to 4.6 km with a Vp of 3.5-5.5 km/s, a Vs of 1.9-3.1 km/s, and Vp/Vs ratios of 1.71-1.76, indicating a low porosity and high degree of diagenesis. High-velocity lower crust (HVLC) is imaged in our model, with a Vp of 7.0-7.5 km/s +/- 0.05-0.25 km/s and Vp/Vs ratios of 1.70-1.82 +/- 0.05. The composition of the HVLC is mainly mafic, we considered it is related to magmatic underplating due to decompression melting caused by crustal extension. The crustal anomalies with high Vp/Vs ratios of 1.80-1.85 +/- 0.04 are identified, which are the product of post-rift magmatic intrusions. The seaward increase in continental lower crustal Vp/Vs ratios, suggests an increasing level of mafic intrusion into the continental crust. We attributed crustal hyperextension to increasing fault density, which caused intense magmatic intrusion and thinner HVLC beneath the continent-ocean transition (COT).

Automated summary

The northern continental margin of the South China Sea is a unique rifted margin with complex relationships between crustal extension and magmatism. High-velocity lower crust (HVLC) composed mainly of mafic materials is attributed to magmatic underplating caused by decompression melting. Crustal anomalies with high Vp/Vs ratios are identified as products of post-rift magmatic intrusions, indicating an increasing level of mafic intrusion into the continental crust.