georefid:2013-001090SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2013-07-08T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1016/j.epsl.2012.06.0482012-01-01publicationgeorefid:2013-001090doi:10.1016/j.epsl.2012.06.048Marcaillou, BorisUniversite des Antilles et de la Guyane, EA LaRGe, Guadeloupe, FranceauthorHenry, PierreCollege de France, FranceauthorKinoshita, MasatakaJapan Agency for Marine-Earth Science and Technology, JapanauthorKanamatsu, ToshiyaUniversity of Florida, United StatesauthorScreaton, ElizabethRice University, United StatesauthorDaigle, HughUniversity of Tokyo, JapanauthorHarcouet-Menou, VirginieKorea Institute of Geoscience and Mineral Resources, South KoreaauthorLee, YoungminNational Institute of Advanced Industrial Science and Technology, JapanauthorMatsubayashi, OsamuCenter for Deep Earth Exploration, JapanauthorThu, Moe KyawauthorKodaira, ShuichiauthorYamano, MakotoauthorElsevier, Amsterdam, NetherlandspublisherdocumentHardcopyEarth and Planetary Science Letters349-350171-185The location of the seismogenic zone across the To-nankai margin segment has been widely investigated using geodetic, tsunami, seismologic, and heat-flow data as well as thermal models. Seafloor heat-flow measurements show large scatter, raising questions about the thermal state of the incoming and overriding plates. In this study, new temperature and conductivity measurements recorded in the Philippine Sea Plate (PSP) and in the accretionary prism during IODP Expedition 333 are integrated with recent data on the margin structure and seismicity to improve constraints on the thermal structure of the incoming plate and the subduction zone as well as the thermal conditions within the seismogenic zone. IODP Expedition 333 measurements provide heat-flow values that are lower than the average of nearby seafloor measurements. Thermal modeling for the PSP suggests that hydrothermal warming is insignificant in the trench. Thus, an observed widespread positive thermal anomaly in the Shikoku Basin that peaks at the Kashinozaki knoll more likely results from vigorous thermal convection in the upper mantle in back-arc context. The modeled thermal structure of the margin from the trench to the mantle shows a significantly colder interplate contact than in previous studies. The seismogenic zone is likely to be 30-170 km from the deformation front, corresponding to the 100-340 degrees C temperature range. The 1944 co-seismic slip zone extends farther southward where temperatures are about 60 degrees C. Slow-slip earthquakes are located in the downdip transition zone between 340 and 440 degrees C across the intersection of the Moho and the megathrust fault. This improved thermal structure from the trench to the mantle results mainly from a better estimate of oceanic plate age, slab dip and sedimentation rate variations in the trench. This last parameter cools the interplate contact until a depth of approximately 35 km, shifting the thermally defined seismogenic zone landward by approximately 20 km and significantly diminishing its influence near the corner flow area. Abstract Copyright (2012) Elsevier, B.V.completedSolid-earth geophysicsaccretionary wedgesactive faultsback-arc basinsbasinscoseismic processesdeformationearthquakesExpedition 333faultsheat flowIntegrated Ocean Drilling ProgramKashinozaki KnollmantlemodelsMohorovicic discontinuityNanTroSEIZENorth PacificNorthwest Pacificocean floorsPacific OceanPhilippine Sea Plateplate tectonicssedimentation ratesShikoku Basinslow-slip earthquakessubduction zonesthermal anomaliesthermal conductivityTonankai earthquake 1944upper mantleWest Pacificurn:org.iodp:exp:333urnlargerWorkCitationcampaignEnglishgeoscientificInformation135.0000138.000032.000034.0000