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Tectonic inversion events in the western San Jorge Gulf Basin from seismic, borehole and field data
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文摘

The San Jorge Gulf Basin is a Mesosoic rift inverted in its western sector.

Tectonic inversion formed the Bernardides System in the Patagonian foreland area.

The evolution of the western basin domain is analyzed through subsurface data.

Several deformational events uplifted this area beginning in late Early Cretaceous.

Positive inversion was related to a variable horizontal stress direction through time.

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