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dc.contributor.authorGross, Felix-
dc.contributor.authorMountjoy, Joshu-
dc.contributor.authorCrutchle, Garethy-
dc.contributor.authorKoch, Stephanie-
dc.contributor.authorBialas, Jörg-
dc.contributor.authorPecher, Ingo-
dc.contributor.authorWoelz, Susi-
dc.contributor.authorDannowski, Anke-
dc.contributor.authorCarey, Jon-
dc.contributor.authorMicallef, Aaron-
dc.contributor.authorBöttner, Christoph-
dc.contributor.authorHuhn, Katrin-
dc.contributor.authorKrastel, Sebastian-
dc.date.accessioned2019-08-12T10:34:52Z-
dc.date.available2019-08-12T10:34:52Z-
dc.date.issued2016-
dc.identifier.citationGross, F., Mountjoy, J., Crutchle, G., Koch, S., Bialas, J., Pecher, I., ... & Böttner, C. (2016). Submarine creeping landslide deformation controlled by the presence of gas hydrates: The Tuaheni Landslide Complex, New Zealand. Geophysical Research Abstracts , 18en_GB
dc.identifier.issn16077962-
dc.identifier.urihttps://www.um.edu.mt/library/oar/handle/123456789/45490-
dc.description.abstractMethane hydrate occurrence is bound to a finite pressure/temperature window on continental slopes, known as the gas hydrate stability zone (GHSZ). Hydrates within sediment pore spaces and fractures are recognized to act like a cement, increasing shear strength and stabilizing slopes. However, recent studies show that over longer strain periods methane hydrates can undergo ductile deformation. This combination of short term strengthening and longer term ductile behavior is implicated in the development of slow creeping submarine landforms within the GHSZ.en_GB
dc.language.isoenen_GB
dc.publisherCopernicus GmbHen_GB
dc.rightsinfo:eu-repo/semantics/restrictedAccessen_GB
dc.subjectMass-wasting -- New Zealanden_GB
dc.subjectSubmarine topography -- New Zealanden_GB
dc.subjectLandslide hazard analysis -- New Zealanden_GB
dc.subjectMarine sediments -- New Zealanden_GB
dc.subjectTsunamis -- New Zealanden_GB
dc.subjectSubmarine geology -- New Zealanden_GB
dc.titleSubmarine creeping landslide deformation controlled by the presence of gas hydrates : the Tuaheni Landslide Complex, New Zealanden_GB
dc.typearticleen_GB
dc.typeotheren_GB
dc.rights.holderThe copyright of this work belongs to the author(s)/publisher. The rights of this work are as defined by the appropriate Copyright Legislation or as modified by any successive legislation. Users may access this work and can make use of the information contained in accordance with the Copyright Legislation provided that the author must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the prior permission of the copyright holderen_GB
dc.description.reviewedpeer-revieweden_GB
dc.publication.titleGeophysical Research Abstractsen_GB
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