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Lithospheric-scale centrifuge models of pull-apart basins
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Lithospheric-scale centrifuge models of pull-apart basins are presented.

The models possess more realistic boundary conditions than traditional 1 g models.

Basin geometry is controlled by the angle of offset between the master fault segments.

Oblique–slip sidewall faults and cross-basin faults accommodate basin development.

Faulting corresponds at depth to ductile thinning and asthenospheric upwelling.

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