nkysdb: 共著者関連データベース
NAKATA Ryoko 様の 共著関連データベース
+(A list of literatures under single or joint authorship with "NAKATA Ryoko")
共著回数と共著者名 (a list of the joint author(s))
13: NAKATA Ryoko
9: HORI Takane
4: KANEDA Yoshiyuki, SUDA Naoki
3: ARIYOSHI Keisuke, HASEGAWA Akira, HINO Ryota, HYODO Mamoru, MATSUZAWA Toru, TSURUOKA Hiroshi
2: ANDO Ryosuke
1: AMPUERO Jean-Paul, ARAKIEiichiro, IDE Satoshi, KAMIYA Shinichiro, KUSUMI Takehiro, MIYAZAKI Shin'ichi, NAKANO Masaru, SUZUKI Kensuke, TAKAHASHI Narumi
発行年とタイトル (Title and year of the issue(s))
2006: Tidal Synchronicity of the Low Frequency Tremor in Eastern Shikoku, Japan(V41A 1700)
2007: Occurrence of Deep Low frequency Tremors Synchronized to Earth Tides(T12C 05)
2008: Non volcanic tremor resulting from the combined effect of Earth tides and slow slip events
2010: A slip pulse model with fault heterogeneity for low frequency earthquakes and tremor along plate interfaces
2010: An automatic monitoring system for nonvolcanic tremors in southwest Japan
2011: Generation mechanism of slow earthquakes: Numerical analysis based on a dynamic model with brittle ductile mixed fault heterogeneity
2012: Migration process of very low frequency events based on a chain reaction model and its application to the detection of preseismic slip for megathrust earthquakes
2012: Numerical simulation of afterslips and slow slip events that occurred in the same area in Hyuga nada of southwest Japan
2014: A trial derivation of seismic plate coupling by focusing on the activity of shallow slow earthquakes
2014: Possible slip history scenarios for the Hyuga nada region and Bungo Channel and their relationship with Nankai earthquakes in southwest Japan based on numerical simulations
2014: Reproducibility of spatial and temporal distribution of aseismic slips in Hyuga nada of southwest Japan
2014: The detectability of shallow slow earthquakes by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET) in Tonankai district, Japan
2016: Synchronous changes in the seismicity rate and ocean bottom hydrostatic pressures along the Nankai trough: A possible slow slip event detected by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET)