HR: 1340h
AN: T13B-0464    [Abstracts]
TI: The Nankai OOST zone exposed along the Shionomisaki Submarine Canyon - Dive results of YK05-08 Leg 2
AU: Anma, R
T13B-0464 AF: University of Tsukuba, Ten-no dai 1-1-1, Tsukuba, 305-8572 Japan
AU: * Ogawa, Y
T13B-0464 AF: University of Tsukuba, Ten-no dai 1-1-1, Tsukuba, 305-8572 Japan
AU: Moore, G
T13B-0464 AF: University of Hawaii, 1680 East-West Rd., POST 813, Honolulu, HI 96822 United States
AU: Kawamura, K
T13B-0464 AF: Fukada Geological Institute, 2-13-12 Honkomagome Bunkyoku, Tokyo, 113-0021 Japan
AB: The Shionomisaki submarine canyon cuts EW-trending five major ridges developed in the Plio-Pleistocene Nankai accretionary prism. The fifth ridge (numbered from the accretion toe in the south) is an extension of the Omine ridge where the out-of-sequence thrust (Nankai OOST zone) were detected through CDEX seismic profiles. We observed structures developed around the Nankai OOST zone along the canyon slope using submersible Shinkai 6500 during JAMSTEC cruise YK05-08 Leg 2. Three dives in addition to two previous dives (one include transect along the third ridge) verified that Shionomisaki Canyon exposes typical accretionary prism features in sandstone dominant thick turbidite sequences, including regular repetition of offscraping and underplating structure. Only near the Nankai OOST zone, extensive activities of fluid seepages were observed demarcated by the presence of chemosynthetic biocommunities, such as Calyptogena and Vesicomyid clams and Vestimentiferan tube worm. Each dive was designed to start from the canyon bottom, climbing up the canyon slope and end in EW-trending gully developed in the fifth ridge, to obtain a 3D images of the Nankai OOST ridge. Distributions of the chemosynthetic biocommunities were observed in the north of the Nankai OOST ridge suggesting a development of antithetic fault system. The ridge itself was disrupted by numerous EW-trending gullies where Calyptogena colonies were widely distributed. These gullies must correspond to spray faults that were bifurcated form the main OOST fault. Detailed observations on collected specimens revealed developments of web and vein structures together with black seams. Needle test indicated that the rocks in the middle part of the OOST ridge is more consolidated compared to those of the north and south exposures.
DE: 8170 Subduction zone processes (1031, 3060, 3613, 8413)
SC: Tectonophysics [T]
MN: Fall Meeting 2005