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Relations of the reason why upper part mantle across the sedimentation plate of the low temperature is a high temperature and the fact that X-rays occur from a tornado(P3-085)(poster session)(abs.)
MASE Hirofumi
itemdescription
TitleRelations of the reason why upper part mantle across the sedimentation plate of the low temperature is a high temperature and the fact that X-rays occur from a tornado(P3-085)(poster session)(abs.)
AuthorsMASE Hirofumi
Data nameProgramme and Abstracts, the Seismological Society of Japan, Fall Meeting
Volume2007
Page296-296
Year2007
PublisherSeismological Society of Japan
LanguageJA
GEOLIS URLhttps://darc.gsj.jp/archives/detail?cls=geolis&pkey=200741149
@idhttps://gbank.gsj.jp/ld/resource/geolis/200741149