Implication of the temporal sulphur isotopic variation during the 2000 eruption of Miyakejima Volcano, Japan

Island Arc

Volumn 16, Issue 1, 2007, Pages 83-92

  Imai, Akira ^a,b   Geshi, Nobuo ^a,c   Shimano, Taketo ^a,d   Nakada, Setsuya ^a  

^a UNIVERSITY OF TOKYO   (Japan)

^b KYUSHU UNIVERSITY   (Japan)

^c NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^d TOHOKU UNIVERSITY   (Japan)

Author keywords

Eruption; Isotopic fractionation; Miyakejima Volcano; Subvolcanichy drothermal system; Sulphur isotope; Volcanic ash

Indexed keywords

HYDROTHERMAL SYSTEM; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; SULFUR ISOTOPE; TEMPERATURE EFFECT; TEMPORAL VARIATION; VOLCANIC ASH; VOLCANIC ERUPTION; VOLCANOLOGY;

ASIA; CHUBU; EURASIA; FAR EAST; HONSHU; IZU ISLANDS; JAPAN; MIYAKEJIMA; SHIZUOKA [CHUBU];

EID: 33847018068     PISSN: 10384871     EISSN: 14401738     Source Type: Journal    
DOI: 10.1111/j.1440-1738.2007.00549.x     Document Type: Article

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