@article{oai:ir.kagoshima-u.ac.jp:00012973,
 author = {福井, 海世 and FUKUI, Miyo and 小林, 励司 and KOBAYASHI, Reiji and 後藤, 和彦 and GOTO, Kazuhiko},
 journal = {鹿児島大学理学部紀要, Reports of the Faculty of Science, Kagoshima University},
 month = {Dec},
 note = {During the passage of waves from the 2011 off the Pacific coast of Tohoku earthquake (MW 9.0),
early post-earthquakes have been observed over the Japanese Islands. Such early post-earthquakes are
considered to be triggered by the main shock of the 2011 off the Pacific coast of Tohoku earthquake. In this
study, we detected triggered earthquakes in Kyushu more carefully by using more seismic stations than
the previous studies. We detected 29 earthquakes, located 15 hypocenters, and determined 2 focal
mechanisms. These events are located volcanic and seismic areas. One of the focal mechanisms differs from
those of the background seismicity. We infer that the dynamic stress changes due to the seismic waves may
differ from the background stress field.},
 pages = {31--41},
 title = {2011年東北地方太平洋沖地震により動的に誘発された九州の地震},
 volume = {45},
 year = {2012}
}