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佐藤, 時治郎 ; 渡辺, 俊三
概要:
日本脳卒中学会第7回(1982年5月20日, 弘前市), 特別講演 IV
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| 2.
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福島, 裕
概要:
第36回東北学校保健学会(1988年9月10日, 弘前市)
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| 3.
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氏家, 良博
概要:
The borehole was drilled 1000 m through sandstones, siltstones and tuff of Quaternaryto Neogene Tertiary age at 40 0 35'N, 1400 30'E in Hirosaki City. Kerogens separatedfrom slimes were characterized by elemental analysis, IH-NMR
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and infrared spectroscopy.It is assumed from the elemental analyses that these kerogens may be derivedfrom a mixture of pollen, spore, plankton, bacteria and terrestrial higher plant.But any parameter in elemental composition, spin-lattice relaxation time CT1) of JH_NMR and infrared spectra shows no reasonable change due to burial diagenesis. Itis considered that these phenomena came out because slimes whoes kerogens wereanalyzed had been contaminated by younger sediments caved in from well walls andcontained in mud filtrate, and/or by older sediments resedimented from lower horizon.
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| 4.
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氏家, 良博
概要:
The Akiyoshi Limestone Group of Carboniferous to late Permian age composesthe Akiyoshi Limestone Plateau in Yamaguchi Prefecture, the west end of Honshu, Japan.Kerogens from limestones and interbedded black shales of the Akiyoshi
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LimestoneGroup were examined by elemental analysis and infrared spectroscopy. Limestonesmainly include kerogens of type III accompanied by type II whose origins have notbeen clarified. Black shales interbedded by limestones contain kerogens with extremelylow HIC ratio. The kerogens in black shales are infered to be "residual" materialswhich comprise contemporaneously oxidized and older recycled matter.
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安野, 眞幸
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安野, 眞幸
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安野, 眞幸
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安野, 眞幸
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| 9.
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太田, 尚充
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| 10.
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太田, 尚充
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