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How used TanDEM-X Radar Interferometry to detect magma transport and quantify eruptive volumes : the example of 2011 Nyamulagira eruption (D.R. Congo)

dc.contributor.authorAlbino, F.
dc.contributor.authorKervyn, F.
dc.contributor.authorSmets, B.
dc.contributor.authord'Oreye, N.
dc.date2013
dc.date.accessioned2016-03-15T10:05:40Z
dc.date.available2016-03-15T10:05:40Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/1801
dc.languageeng
dc.titleHow used TanDEM-X Radar Interferometry to detect magma transport and quantify eruptive volumes : the example of 2011 Nyamulagira eruption (D.R. Congo)
dc.typeConference
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeNatural hazards
dc.source.titleActive Volcanism and Continental Rifting with special focus on the Kivu rift zone (AVCoR 2013), Gisenyi, Rwanda, November 12-14 2013
Orfeo.peerreviewedNo
dc.identifier.rmca3445


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