Art

J-GLOBAL ID：201102223834008725   Reference number：11A0181247

Origin of methane in subseafloor geofluid systems

海底下地殻内流体系のメタンの起源

Author (2)： KAWAGUCHI SHINSUKE (海洋研究開発機構) ,  TOKI TOMOHIRO (琉球大 理)
Material： 地球化学
Volume： 44  Issue： 4  Page： 137-154  Publication year： Dec. 25, 2010 
JST Material Number： G0754A  ISSN： 0386-4073  Document type： Article
Article type： 文献レビュー  Country of issue： Japan (JPN)  Language： JAPANESE (JA)

Thesaurus term： *hydrothermal system ,  leaching ,  earth crust ,  fluid ,  *methane gas ,  carbon isotope ,  isotopic ratio ,  hydrogen isotope ,  *sea bed
Semi thesaurus term： genesis

JST classification (2)： Other isotopic geochemistry  (MC03020J) ,  Geochemistry of lithosphere in general  (DD01041C)

Reference (101)：

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• BELAY, N. Ethane production by Methanosarcina Barkeri during growth in ethanol supplemented medium. Antonie Van Leeuwenhoek Journal of Microbiology. 1988, 54, 113-125
• BERNER, U. Primary cracking of algal and landplant kerogens : Kinetic models of isotope variations in methane, ethane and propane. Chemical Geology. 1995, 126, 233-245
• BLAIR, N. E. The carbon isotope biogeochemistry of acetate from a methanogenic marine sediment. Geochimica et Cosmochimica Acta. 1992, 56, 1247-1258
• BLANK, J. G. The concentration and isotopic composition of carbon in basaltic glasses from the Juan-de-Fuca Ridge, Pacific-Ocean. Geochimica et Cosmochimica Acta. 1993, 57, 875-887

Terms in the title (5)： 海底 ,  地殻 ,  流体 ,  メタン ,  起源