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Structural evolution of the inverted Neoproterozoic Yeneena Basin, Australia
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DOI：10.1016/j.precamres.2026.108127.png)
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Abstract
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• Basin inversion produced folds with predominantly NW-SE trending hinge lines, • During basin inversion, normal faults were reactivated as reverse faults. • Folding dominantly accommodated shortening rather than reverse faulting. • Restoration indicates horsts that segmented the basin into smaller subbasins.
Keywords:
Yeneena basin
Structural reconstruction
Basin evolution
Balanced cross-section
Sedimentary-hosted mineral systems
Copper
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