Earthquake Recurrences Since Late Pleistocene in Nankai Trough of Kumano  

作　　者：Tao Jiang~1,Shenghua Li~2,Chunfeng Li~3,Xinong Xie~1,Xin Su~4,Jianye Ren~1 1.Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences(Wuhan),Wuhan 430074,China. 2.Department of Earth Sciences,University of Hong Kong,Pokfullam Road,Hong Kong,China 3.School of Ocean and Earth Sciences,Tongji University,Shanghai 200092,China 4.School of Marine Geosciences,China University of Geosciences(Beijing),Beijing 100083,China 

出　　处：《地学前缘》2009年第S1期221-221,共1页Earth Science Frontiers

基　　金：supported both by J-DESC(Japan Drilling Earth Science Consortium);the National Natural Science Foundations of China(No.40806019 and 40876022)

摘　　要：The Nankai Trough has a 1300-year record of generating large earthquakes(M_w】8)with a recurrence time of～100-200 a,but unfortunately,we don’t know the frequency of earthquakes before.Results from recent expeditions of NanTroSEIZE Stage 1 IODP 314/315/316 recovered many cycles of turbidites since late Pleistocene,which are triggered during the past earthquake shaking.Our purpose is

关 键 词：EARTHQUAKE SEIZE IODP TURBIDITE OSL 

分 类 号：P315[天文地球—地震学]