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Figure F33. Normal fault displacement of a bed within the forearc basin (649 m LWD depth below seafloor [LSF]). The fracture cannot clearly be seen, but its azimuth and dip can be estimated from the displacement. Breakouts oriented northwest–southeast are clearly seen as conductive vertical lines 180° apart. Static normalization shallow resistivity image. 3-D = three-dimensional, tadpole lines = dip direction of the plane.

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