Abstract

Fine-grained mass-transport deposits (MTDs), especially their compressional toe zones, are traditionally considered as effective seal in constraining the vertical fluid migration underneath. However, this study documents thrust faults at the compressional toe zone of fine-grained MTDs that could disaggregate the seal competence and promote vertical fluid flow. The investigated MTD referred to as MTD-a lies directly over a large hydrocarbon reservoir that is located within the Central Canyon of northern South China Sea, which is examined by using high-resolution 3D seismic and borehole data. Thrust faults and irregular blocks composed of coarse-grained sandstones are observed in the compressional zone of the MTD-a’s toe. More importantly, seismic evidence (e.g., enhanced seismic reflections) suggests that a large amount of hydrocarbons from the underlying reservoir penetrated through the MTD-a along these thrust faults and charged into the coarse-grained sandstone blocks. This clear evidence of thrust faults compromising the MTD’s seal effectiveness and thus facilitating the vertical fluid flow through the non-permeable strata demonstrate the importance of reassessing the seal capacity of MTD.

Highlights

  • Mass-transport deposits (MTDs) widely occur at the continental margins and island flanks

  • Multiple mass-transport deposits (MTDs) characterized by chaotic/blanking seismic reflections are observed above the Central Canyon, separated by continuous seismic surfaces (Figures 3A, 5, 6)

  • This study is focused on the lowermost MTD, here named as MTD-a, which is directly draped on the Central Canyon (Figure 3A)

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Summary

Introduction

Mass-transport deposits (MTDs) widely occur at the continental margins and island flanks They are usually composed of the headwall domain, translational domain, and toe domain (Martinsen, 1994; Lastras et al, 2002) and, a systematic distribution of strain transferred from extensional structures in the headwall zone to compressional structures in the toe zone (Trincardi and Argnani, 1990; Canals et al, 2004; Frey Martinez et al, 2005). The long-distance transportation of failed sediments at the toe zone is typically highly deformed and their fabrics are greatly damaged These make the seal capacity of compressional toe zones of MTDs more effective. Remnant blocks within MTDs are proposed to provide conduits for the vertical fluid flows (Alves et al, 2014; Gamboa and Alves, 2015; Cox et al, 2020), no vertical flow pathways have been identified at the compressional toe zone until now

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