Submarine Outcrop Evidence for Transpressional Deformation Within the Nankai Accretionary Prism, Tenryu Canyon, Japan - Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin - page 204

Table 1 (continued)
Dive Strike Dip Dip direction Type

0 60 E Bedding

330 45 E Bedding

232 60 NW Bedding

20 70 E Bedding

245 70 NW Bedding

Dive 1058 285 10 NE Bedding

315 10 NE Bedding

285 15 NNE Bedding

315 15 E Bedding

300 10 N Bedding

330 30 NE Bedding

255 20 N Bedding

20 10 E Bedding

290 10 N Bedding

260 15 N Bedding

325 20 N Bedding

0 20 E Bedding

290 20 N Bedding

270 10 N Bedding

270 5 N Bedding

250 15 N Bedding

30 15 E Bedding

340 20 E Bedding

270 15 N Bedding

45 15 E Bedding

124 70 W Joint

35 70 E Joint

145 80 N Joint

280 90 - Joint

330 90 - Joint

150 60 W Joint

320 90 - Joint

200 90 - Joint

290 90 - Joint

200 80 W Joint

120 20 S Fault

325 90 - Fault

15 90 - Fault

310 90 - Fault

330 90 - Fault

dives 886 and 892, respectively, and therefore were deposited in Early to Middle
Pleistocene. Age constraints on sediments observed on Dive 1058 are not readily avail-
able, but range from Early Pliocene and could be as young as <0.18 Ma, based on
biostratigraphic ages of the sediments near the frontal thrust (Kawamura et al. 2009 ).
Shipboard uniaxial compression strength measurements show that the samples
collected on Dives 1056, 1057, and 1058 are relatively weak, poorly consolidated