摘要
Systematic paleomagnetic,rock magnetic and sedimentological analyses were undertaken in core KCES(35°56.150’N,130°41.915’E,water depth of 1 463.8 m,total length of 10.3 m) of Ulleung Basin,Japan Sea for the last 48 ka.The rock magnetic evolution in core KCES has the potential to record changes of terrigenous input,bottom current and post-depositional modification which could correspond with the well known millennial events.