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dc.contributor.authorHarja, A.en
dc.contributor.authorSrigutomo, W.en
dc.contributor.authorTanaka, Y.en
dc.contributor.authorKagiyama, T.en
dc.contributor.authorSutarno, D.en
dc.contributor.alternative鍵山, 恒臣ja
dc.date.accessioned2016-03-29T06:49:34Z-
dc.date.available2016-03-29T06:49:34Z-
dc.date.issued2016-01-19-
dc.identifier.issn1755-1307-
dc.identifier.urihttp://hdl.handle.net/2433/209900-
dc.description.abstractShallow resistivity structure around Nakadake craters has been revealed by extensive VLF- MT survey from August to October 2006. This structure comprises a varied resistivity value at the upper and bottom layer of the western flank of craters; a conductive upper layer at the fourth Crater; and a resistive upper layer at southern part of craters. The conductive value of second layer at a line in the western flank and southern part of craters at several ten meter depth, interpreted as water saturated, and high resistivity at second line of western flank of craters as sheet of lava and at fourth crater is interpreted as lava rock. At western flank of craters, we found the resistivity value and the depth of second layer decrease in depth with decreasing of distance to craters line.en
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherInstitute of Physics Publishingen
dc.rightsPublished under licence in Journal Title by IOP Publishing Ltd. Content from this work may be used under the terms of the Creative Commons Attribution 3.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.en
dc.titleVLF -MT Survey around Nakadake crater at Aso Volcanoen
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.jtitleIOP Conference Series: Earth and Environmental Scienceen
dc.identifier.volume29-
dc.relation.doi10.1088/1755-1315/29/1/012016-
dc.textversionpublisher-
dc.identifier.artnum012016-
dcterms.accessRightsopen access-
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