that these knolls are monogenetic volcanoes. Olivine basalts were sampled in Dive #, and clinopyroxene basalts were sampled in Dive #. The eastern wal
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1 YK- # ## # # # #, #, #, #, # #, # Submersible study around the Sofugan Tectonic Line, Izu-Bonin Arc Toshiya FUJIWARA Makoto YUASA Teruo WATANABE Kiyoaki NIIDA Akira NISHIMURA Izumi SAKAMOTO Osamu ISHIZUKA Makiko IMAMURA Kaoru TSUKUDA We conducted submersible surveys around the Sofugan Tectonic Line, Izu-Bonin Arc, western Pacific, during the "Yokosuka/Shinkai " YK- cruise. Hornblende dacite and diorite porphyrite rocks were sampled from the western wall of Ohmachi Seamount in Dive #. Upper mantle-derived and cumulate-derived serpentinites were widely exposed at the base of western wall of the Ohmachi Seamount in Dive # and #. Some samples are considerably fresh and containing primary pyroxenes and olivines. The small knolls located in the back-arc region in the northwest of the Sofugan Tectonic Line, the seafloor appeared to be composed of pillow lavas, sheet lavas, and pyroclastic rocks, however thick manganese crust prevented visual observation. The slopes were almost constant through the dive tracks, therefore there was no evidence of lateral eruption. This suggests Japan Marine Science and Technology Center Geological Survey of Japan Hokkaido University Nippon Marine Enterprises
2 that these knolls are monogenetic volcanoes. Olivine basalts were sampled in Dive #, and clinopyroxene basalts were sampled in Dive #. The eastern wall of Bunka Seamount of the Nishi-shichito Ridge was wholelly covered by thick manganese crust, which protected sampling work, in Dive #. Two dives were devoted to western and eastern walls in a deep graben located in the southwest of Tempo Seamount. These walls were covered with thick sediments and manganese crust, and we could not observe and sample the seafloor rocks which were considered to be the island-arc crust below the cliff of Sofugan Tectonic Line. Small gaps and fissures which cut sediment were observed. These suggest recent tectonic activity. Keywords : Izu-Bonin Arc, Sofugan Tectonic Line, Island Arc, Rift Yuasa, Suyehiro et al., ; Taira et al., a b, Ma Yuasa, Sakamoto et al.,,,, kmm Sakamoto et al., 35 N Honsyu 30 N Bonin Is. Bunka Smt. Sofugan Tectonic Line Shikoku Basin Knolls Kayo Smt. Getsuyo Smt. 25 N 135 E 140 E Tempo Smt. Oomachi Smt 'E 'E 'E 'E 'E 29 30'N 29 00'N 28 30'N South Doyo Smt 'N 27 30'N 28 00'N Kinyo Smt. Suiyo Smt. East Mokuyo Smt 'N 26 00'N Kaikita Smt. Fig. Location map of around the Sofugan Tectonic Line, Izu-Bonin Arc.
3 Fujiwara et al., YK- Leg ## YK- Leg #, #, # #, # # #, # #, #, #, #, # #, # m :-::-: IGRF LaCoste & Romberg S-. mgal. mgal SeaBeam # # # # NE NW #kmmnw #kmm # # ## # # LaCoste & Romberg G-
4 YK- Leg Fig. Bathymetric map of the survey area. Circles show dive points of previous surveys. Stars show dive points of the YK- Leg cruise.
5 YK- Leg Fig. Survey ship tracks of R/V Yokosuka. Red lines indicate the tracks during the YK- Leg cruise. # #, # YK- m YK- Leg Fig. Bathymetric map around the back-arc small knolls. Contour interval is m. Stars show dive points of the YK- Leg cruise. Fujiwara, T., T. Yamazaki, and M. Joshima: Bathymetry and magnetic anomalies in the Havre Trough and southern Lau Basin: From rifting to spreading in back-arc basins, Earth Planet. Sci. Lett., -, -. Geological Survey of Japan GSJand Coordinating Committee for Coastal and Offshore Geoscience Programmes in East and Southeast AsiaCCOP: Magnetic anomaly map of east Asia :,, CD- ROM Version. JAMSTEC, -. P. A. Jarvis YK- JAMSTEC, -.
6 # #m Fig. Bathymetric map of the # knoll (right) and the # knollleft. Contour interval is m. Circles show rock sampling sites. K#RK#Rol=cpx=pl= ves= Photo Photographs of sample and thin section of K#Rleftand K#Rright. ol=olivine, cpx=clinopyroxene, pl=plagioclase, ves=vesicle.
7 Table Tables of sampling rock descriptions.
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12 Table Table of seafloor gravity measurements. K#RK#R Table Table of density and magnetization measurements of sampling rocks K#R and K#R. Sakamoto, I., T. Fujiwara, O. Ishizuka, and M. Yuasa: Geology and tectonics of the Sofugan Tectonic Line, central part of Izu-Ogasawara Arcabstract, EOS Trans. AGU,, WPGM Suppl.,. Suyehiro, K., N. Takahashi, Y. Ariie, Y. Yokoi, R. Hino, M. Shinohara, T. Kanazawa, N. Hirata, H. Tokuyama, and A. Taira: Continental crust, crustal underplating, and low-q upper mantle beneath an oceanic island arc, Science,, -. Taira, A., S. Saito, K. Aoike, S. Morita, H. Tokuyama, K. Suyehiro, N. Takahashi, M. Shinohara, S. Kiyokawa, J. Naka, and A. Klaus: Nature and growth rate of the northern Izu-BoninOgasawaraarc crust and their implications for continental crust formation, Island Arc,, -. Yuasa, M.: Sofugan Tectonic Line, a new tectonic boundary separating northern and southern parts of the OgasawaraBoninarc, northwest Pacific, in Formation of Active Ocean Margins, edited by N. Nasu, K. Kobayashi, S. Uyeda, I. Kushiro, and H. Kagami, -, Terra Scientific Publishing Company, Tokyo. -, -. -, -. #JAM- STEC, -., -.
Km Km - Yuasa, Sakamoto et al,.. m WGS YK- JAM- STEC, YK- JAMSTEC, YK- JAMSTEC, YK- YK- Jarvis Jarvis YK- - Km. Km Km m m m m m /m Yuasa et al. NW Km
Topographical and geological characteristics of Sofugan Tectonic Line (STL) area, Izu-Ogasawara Arc. Izumi SAKAMOTO Toshiya FUJIWARA and Osamu ISHIZUKA Sofugan Tectonic Line STL locates on the middle part
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