Deformation within the Pisco Basin sedimentary record (southern Peru): Stratabound orthogonal vein sets and their impact on fault development
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文摘

Field-scale deformation features affecting the forearc, Pisco Basin strata.

Structural evolution seem partly independent of plate tectonics.

Normal faults as an evolution of stratabound, orthogonal vein sets.

Normal fault patterns depending on the local σ2/σ3 magnitude ratio.

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