論文- 掛川 武 -
表示方法: 表示形式: 表示順:
件数:78件
[2004]
61.GEOCHEMISTRY OF NITROGEN IN VOLCANIC ROCKS ALTERED BY SUBMARINE HYDROTHERMAL ACTIVITIES AT THE SUIYO SEAMOUNT, IZU-OGASAWARA ARC, JAPAN.[0,vol.1,(2004),153-156]Noda M, Kakegawa T
62.微生物学と地球科学のわかちがたい関係.[科学,74(2),(2004),166-169]遠藤一佳.南澤究.掛川武.犬伏和之
[2003]
63.A novel lineage of sulfate-reducing microorganisms: Thermodesulfobiaceae fam. nov., Thermodesulfobium narugense, gen. nov., sp. nov., a new thermophilic isolate from a hot spring.[Extremophiles,7,(2003),283-290]Mori K., Kim H., Kakegawa T., Hanada S.
64.初期地球環境下での微生物進化.[日本惑星科学会、遊星人,(3),(2003),14-18]掛川武
65.最古の岩石が秘める生命起源へのヒント.[化学,58(7),(2003),30-31]掛川 武
66.Stratigraphic carbon isotope fluctuations of detrital woody materials during the Aptian Stage in Hokkaido, Japan: Comprehensive δ13C data from four sections of the Ashibetsu area.[0,21,(2003),835-847]Ando A. Kakegawa T. Takashima R. Saito T
[2002]
67.Geochemical Cycles of Bio-essential elements on the early Earth and their relationships to origin of life.[Resource Geology,(52),(2002),83-89]Takeshi Kakegawa, Nannri, Noda
68.New perspective on Aptian carbon isotope stratigraphy: Data from d13C records of terrestrial organic matter.[Geology,30(3),(2002),227-230]Ando Atsushi, Takeshi Kakegawa
69.Activities of early life in the Archean oceans: influence from submarine hydrothermal activities.[origin of life and geochemistry,(2002),50-63]Takeshi Kakegawa
[2001]
70.Biological activities and evolution of life during early stage of the Earth history: constraints from the stable isotope records.[Viva Origino,(28),(2001),191-208]Takeshi kakegawa
[2000]
71.Sulfur and carbon isotope analyses of the 2.7 Ga Jeerinah Formation, Fortescue Group, Australia.[Geochemical Journal,(34),(2000),121-133]Takeshi Kakegawa, Kasahara, Ohmotto
72.Biological activities and evolution of life during early stage of the Earth history : Constraints from the stable isotope records.[Viva Origino,28(4),(2000),191-]KAKEGAWA Takeshi
[1999]
73.Sulfur isotope evidence for the origin of 3.4 and 3.1 Ga pyrite at the Princeton Gold Mine, Barberton Greenstone Belt, South Africa.[Precambrian Research,(96),(1999),209-224]KAKEGAWA Takeshi
74.Geochemistry of the 2.O Ga Rove Formation, Canada, suggests an early establishment of the modern style elemental cycles mediated by biological activities.[Geological Society of America, annual meeting, Abstract with program,(118),(1999)]KAKEGAWA Takeshi
[1998]
75.Origins of pyrites in the~2.5Ga Mt. McRae Shale, the Hamersley District, Western Australia.[Geochimica Cosmochiemica Acta,(62),(1998),3205-3220]川井元、大本洋
76.High activity of sulphate-reducing bacteria in Archean and Proterozoic oceans and an early development of the Phanerozoic-style sulphur cycles.[Mineralofical Magazine,(62A),(1998),738-739]KAKEGAWA Takeshi
[1997]
77.カナダニューファウンドランド島チャペルアイランド層における堆積岩の硫黄同位体地球化学.[アメリカ地質学会誌,29(6),(1997),116-]掛川 武
[1993]
78.3.4-billion-year-old biogenic pyrites from Barberton, South Africa: Sulfur isotope evidence.[Science,262,(1993),555-557]H.Ohmoto, D. Lowe and Kakegawa T
Page: [prev] [1] [2] [3] [4]
戻るこのページのトップへ
copyright(c)2005 Tohoku University