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Continental deformation accommodated by non-rigid passive bookshelf faulting: An example from the Cenozoic tectonic development of northern Tibet
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文摘

We propose a non-rigid passive bookshelf-fault model for deformation in north Tibet.

Right-lateral shear drives clockwise rotation and left-slip faulting on W–E faults.

Clockwise rotation of faults occurs against left-slip Altyn Tagh bounding fault.

Model explains bidirectional decrease in slip and four-quadrant strain pattern.

Protracted deformation in northern Tibet since Eocene

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