Turbulent transport and deposition of the Ito pyroclastic flow: Determinations using anisotropy of magnetic susceptibility

Journal of Geophysical Research: Solid Earth

Volumn 102, Issue B10, 1997, Pages 22565-22586

  Baer, E M ^a,b   Fisher, R V ^b   Fuller M ^b   Valentine, G ^c  

^a Highline Community College   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

^c LOS ALAMOS NATIONAL LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ANISOTROPY OF MAGNETIC SUSCEPTIBILITY; DEPOSITION; PYROCLASTIC FLOW; TURBULENCE;

JAPAN, KYUSHU;

EID: 0031416582     PISSN: 21699313     EISSN: 21699356     Source Type: Journal    
DOI: None     Document Type: Article

References (5)

1. Aramaki, S., Geology and pyroclastic flow deposits of the Kokubu area, Kagoshima Prefecture, J. Geol. Soc. Jpn., 75, 425-442, 1969.
2. Aramaki, S., Hydrothermal determination of temperature and water pressure of the magma of Aira caldera, Jpn.. Am. Mineral., 56, 1760-1768, 1971.
3. Aramaki, S., The Aira Caldera and Ito pyroclastic flow, Earth Mon., 5, 64-72, 1983.
4. Aramaki, S., Formation of the Aira Caldera, southern Kyushu, ∼22,000 years ago, J. Geophys. Res., 89, 8485-8501, 1984.
5. Aramaki, S., and T. Ui, The Aira and Ata pyroclastic flows and related calderas and depressions in southern Kyushu, Jpn. Bull. Volcanol. Ser., 2, 29-72, 1966a.