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
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》
EI
CAS
CSCD
北大核心
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)
