georefid:2009-038472georefid:2009-038470SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2204/iodp.proc.314315316.102.20092008-01-01publicationgeorefid:2009-038472doi:10.2204/iodp.proc.314315316.102.2009Moore, Gregory F.Japan Agency for Marine-Earth Science and Technology, Institute for Research on Earth Evolution, Yokohama, JapanauthorPark, J. O.University of Wisconsin-Madison, United StatesauthorBangs, N. L.Ecole Nationale Superieure de Geologie, FranceauthorGulick, Sean P.Chungnam National University, South KoreaauthorTobin, Harold J.CEREGE-College de France, FranceauthorNakamura, Y.University of Texas at Austin, United StatesauthorSato, S.CSIC/Institute of Earth Sciences, SpainauthorTsuji, T.University of Southampton, United KingdomauthorYoro, T.Kyoto University, JapanauthorTanaka, H.University of California-Santa Cruz, United StatesauthorUraki, S.University of Tokyo, JapanauthorKido, Y.Rice University, United StatesauthorSanada, Y.University of Leicester, United KingdomauthorKuramoto, S.Universite de Cergy-Pontoise, FranceauthorTaira, A.Leibniz Institute of Marine Sciences, Federal Republic of GermanyauthorIODP Management International, Washington, DC, United StatespublisherdocumentDigitalIn: Kinoshita, Masataka, Tobin, Harold J., Thu, Moe Kyaw, Gaillot, Philippe, Bourlange, Sylvain, Chang, Chandong, Conin, Marianne, Gulick, Sean P., Jurado Rodriguez, Maria Jose, Martin, Kylara M., McNeill, Lisa, Miyakawa, Ayumu, Moore, J. Casey, Nakamura, Yasuyuki, Saito, Saneatsu, Sawyer, Dale S., Tudge, Joanne, Yamada, Yasuhiro, Ashi, Juichiro, Lallemant, Siegfried, Masago, Hideki, Behrmann, Jan H., Boeckel, Babette, Byrne, Timothy, Calves, Gerome, Famin, Vincent, Guo, Junhua, Hashimoto, Yoshitaka, Hayashi, Hiroki, Henry, Pierre, Hirono, Tetsuro, Hulme, Samuel M., Kaksonen, Anna Henriikka, Kanagawa, Kyuichi, Kanamatsu, Toshiya, Kopf, Achim, Lewis, Jonathan C., Likos, William John, Pares, Josep Maria, Saito, Hiroyuki, Schmidt-Schierhorn, Friederike, Tomaru, Hitoshi, Underwood, Michael, Zhu, Wen-Lu, Kimura, Gaku, Screaton, Elizabeth J., Curewitz, Daniel, Chester, Frederick, Fabbri, Olivier, Fergusson, Chris, Girault, France E., Goldsby, David, Harris, Robert, Inagaki, Fumio, Jiang, Tao, Kitamura, Yujin, Knuth, Matt, Li Chun-Feng, Liljedahl, Lillemor Claesson, Louis, Laurent, Milliken, Kitty, Nicholson, Uisdean, Riedinger, Natascha, Proceedings of the Integrated Ocean Drilling Program; NanTroSEIZE Stage 1; investigations of seismogenesis, Nankai Trough, Japan; Expeditions 314, 315, and 316 of the riser drilling platform from and to Shingu, Japan; Sites C0001-C0006, 21 September-15 November 2007, and sites C0001 and C0002, 16 November-18 December 2007, and sites C0004 and C0006-C0008, 19 December 2007-5 February 2008314/315/316The location of the Integrated Ocean Drilling Program's (IODP) Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) was based on regional two-dimensional seismic reflection surveys carried out by the Japan Agency for Marine-Earth Science and Technology (JAMSTEC). Final site locations were chosen based on a three-dimensional (3-D) seismic reflection survey acquired across the seaward margin of Kumano Basin and the accretionary prism from the basin to the deformation front. This survey covered a region 12 km wide (approximately parallel to the regional structural strike) and 56 km long (approximately perpendicular to the regional strike) and provided detailed images of the structure and seismic stratigraphy of the drill sites. Sites were drilled in the frontal thrust zone at the toe of the accretionary prism, the frontal region of the megasplay fault zone, and the forearc basin. The 3-D seismic data volume images a main frontal thrust at the prism toe with the hanging wall thrust at least 7.5 km seaward over the trench. This configuration is different from that in other parts of the Nankai prism. At the shallow end of the megasplay, the data images a complex thrust system that truncates older structures in the underlying accretionary prism and shows that the hanging wall block has overridden more than 1250 m of young slope sediments. At the forearc basin site, we interpret landward-dipping forearc basin strata onlapping older slope sediments, which in turn overlie an older part of the accretionary prism.completedStratigraphyStructural geologyApplied geophysicsaccretionary wedgesbasin analysisbasinsboreholesCenozoiccorescrustdeep drillingdrillingExpedition 314Expedition 315Expedition 316faultsfore-arc basinsgeophysical methodsgeophysical profilesgeophysical surveysIntegrated Ocean Drilling ProgramIODP Site C0001IODP Site C0002IODP Site C0003IODP Site C0004IODP Site C0008marine drillingmarine sedimentsNankai TroughNankai Trough Seismogenic Zone ExperimentNorth PacificNorthwest Pacificocean floorsoceanic crustPacific Oceansedimentsseismic methodsseismic profilesseismic stratigraphysubduction zonessurveysWest Pacificurn:org.iodp:exp:314urnlargerWorkCitationcampaignurn:org.iodp:exp:315urnlargerWorkCitationcampaignurn:org.iodp:exp:316urnlargerWorkCitationcampaignurn:org.iodp:exp:314:site:C0001urnlargerWorkCitationstudyurn:org.iodp:exp:314urnlargerWorkCitationcampaignurn:org.iodp:exp:315:site:C0001urnlargerWorkCitationstudyurn:org.iodp:exp:315urnlargerWorkCitationcampaignurn:org.iodp:exp:315:site:C0002urnlargerWorkCitationstudyurn:org.iodp:exp:315urnlargerWorkCitationcampaignurn:org.iodp:exp:316:site:C0004urnlargerWorkCitationstudyurn:org.iodp:exp:316urnlargerWorkCitationcampaignurn:org.iodp:exp:316:site:C0008urnlargerWorkCitationstudyurn:org.iodp:exp:316urnlargerWorkCitationcampaignEnglishgeoscientificInformation136.3800136.434033.124433.1800Includes appendicesapplication/pdfunknownSEDIS Publication Catalogue

ana.macario@awi.de

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