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dc.contributor.authorKluger, Michalen_NZ
dc.contributor.authorSeibel, D.en_NZ
dc.contributor.authorMoon, Vicki G.en_NZ
dc.contributor.authorKreiter, S.en_NZ
dc.contributor.authorHepp, D.A.en_NZ
dc.contributor.authorde Lange, Willem P.en_NZ
dc.contributor.authorJorat, Ehsanen_NZ
dc.contributor.authorMörz, T.en_NZ
dc.coverage.spatialBremenen_NZ
dc.date.accessioned2015-10-07T19:52:06Z
dc.date.available2015-09-07en_NZ
dc.date.available2015-10-07T19:52:06Z
dc.date.issued2015-09-07en_NZ
dc.identifier.citationKluger, M., Seibel, D., Moon, V. G., Kreiter, S., Hepp, D., de Lange, W. P., … Mörz, T. (2015). The role of halloysite morphology on undrained shear strength and sensitivity of volcanic ashes in New Zealand. Presented at the InterCoast Workshop, Bremen.en
dc.identifier.urihttps://hdl.handle.net/10289/9676
dc.description.abstractLarge areas of the North Island of New Zealand are covered by thick Pleistocene pyroclastic deposits that are often prone to coastal landslides. In the Tauranga region (Fig. 1a) some landslides are associated with the Pahoia Tephras, a sequence of highly weathered sensitive rhyolitic ashes containing high amounts of the clay mineral halloysite (Moon et al., 2013, 2015).
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.relation.urihttps://www.marum.de/en/6th_Annual_INTERCOAST_Workshop.html
dc.rights© 2015 the authors
dc.sourceInterCoast Workshopen_NZ
dc.titleThe role of halloysite morphology on undrained shear strength and sensitivity of volcanic ashes in New Zealanden_NZ
dc.typeConference Contribution
pubs.elements-id130264
pubs.finish-date2015-09-18en_NZ
pubs.start-date2015-09-07en_NZ


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