Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough
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文摘

Backstop can be identified from deformation features of forearc basin sequence.

Static backstop is generated by age difference from hiatus in subduction process.

The igneous activity in middle Miocene contributes to originate lithified backstop.

Backstop controls fault system within accretionary prism including ancient splay fault.

Backstop distribution could relate to the coseismic rupture segment.

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