Please use this identifier to cite or link to this item: https://www.um.edu.mt/library/oar/handle/123456789/45490
Title: Submarine creeping landslide deformation controlled by the presence of gas hydrates : the Tuaheni Landslide Complex, New Zealand
Authors: Gross, Felix
Mountjoy, Joshu
Crutchle, Garethy
Koch, Stephanie
Bialas, Jörg
Pecher, Ingo
Woelz, Susi
Dannowski, Anke
Carey, Jon
Micallef, Aaron
Böttner, Christoph
Huhn, Katrin
Krastel, Sebastian
Keywords: Mass-wasting -- New Zealand
Submarine topography -- New Zealand
Landslide hazard analysis -- New Zealand
Marine sediments -- New Zealand
Tsunamis -- New Zealand
Submarine geology -- New Zealand
Issue Date: 2016
Publisher: Copernicus GmbH
Citation: Gross, 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 , 18
Abstract: Methane 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.
URI: https://www.um.edu.mt/library/oar/handle/123456789/45490
ISSN: 16077962
Appears in Collections:Scholarly Works - FacSciGeo

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