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Figure F6. Single-channel seismic lines for J Anomaly Ridge running along-dip, with locations of related Expedition 342 drill sites. Profile KNR 179-1, Line 5, crosses J Anomaly Ridge through DSDP Site 384. Note the thinning of the transparent seismic unit of early?–late Eocene age between crossing Lines 10 and 12, here interpreted as erosional thinning of the carbonate section through the carbonate lysocline. Line 12 crosses Line 5 close to the depth of the CCD.

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