@article{oai:nipr.repo.nii.ac.jp:00002781,
 author = {アカマツ, ジュンペイ and カク, ヒロユキ and カナオ, マサキ and AKAMATSU, Junpei and KAKU, Hiroyuki and KANAO, Masaki},
 journal = {Proceedings of the NIPR Symposium on Antarctic Geosciences},
 month = {Sep},
 note = {P(論文), Coda 〓 of local earthquakes observed at Bomi, southeast Tibetan plateau was evaluated using a single scattering model and compared with that in the Lutzow-Holm Bay region, East Antarctica. The results obtained are : (1) 〓^<-1> for short lapse time (SLT) from 5 to 50s shows large dependence on frequency; (2) 〓^<-1> for SLT in the Tibetan plateau region is larger than that in the Lutzow-Holm Bay region; (3) 〓^<-1> for long lapse time from 80 to 160s in the Tibetan region is nearly the same as that in the Lutzow-Holm Bay region. Although there is a need for discussion of coda excitation modeling, all these features are consistent with the general relation between coda 〓 and regional tectonic activities.},
 pages = {15--24},
 title = {CODA 〓 OF LOCAL EARTHQUAKES OBSERVED ON THE SOUTHEAST TIBETAN PLATEAU : COMPARISON WITH LUTZOW-HOLM BAY REGION, EAST ANTARCTICA},
 volume = {8},
 year = {1995}
}