Geological Characteristics of Mud Volcanoes and Diapirs in the Northern Continental Margin of the South China Sea: Implications for the Mechanisms Controlling the Genesis of Fluid Leakage Structures

<div>Seismic profile of the Dongsha Islands. The seismic profile reveals a thin Cenozoic sedimentary cover, and the uplift of the Mesozoic basement caused the upward deformation of the overlying sediment.</div>

Geofluids

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Figure 6

Figure 6: Geological Characteristics of Mud Volcanoes and Diapirs in the Northern Continental Margin of the South China Sea: Implications for the Mechanisms Controlling the Genesis of Fluid Leakage Structures 

Figure 6 | Geological Characteristics of Mud Volcanoes and Diapirs in the Northern Continental Margin of the South China Sea: Implications for the Mechanisms Controlling the Genesis of Fluid Leakage Structures 