Self-constrained inversion of microgravity data along a segment of the Irpinia fault
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文摘

A self-constrained inversion of gravity data in active fault area is proposed.

The parameters that constrain the inversion come from the analysis of the anomalies.

The obtained models show both the shape of the fault and the overlying sediments.

Reasonable slip rate values can be evaluated on the obtained density models.

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