--> Figure 13. Triangle ā€œUā€ field shows that the magnetic gradients that define basement faults can sometimes be subtle and that better defined faults, as the one 3 miles to the southwest and parallel to the field, are not necessarily the ones that were reactivated.

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Figure 13. Triangle ā€œUā€ field shows that the magnetic gradients that define basement faults can sometimes be subtle and that better defined faults, as the one 3 miles to the southwest and parallel to the field, are not necessarily the ones that were reactivated.