Dynamics of large submarine landslide from analyzing the basal section of mass-transport deposits sampled by IODP Nankai Trough Submarine Landslide History (NanTroSLIDE)

Wednesday, 17 December 2014: 8:00 AM
Michael Strasser, ETH Swiss Federal Institute of Technology Zurich, Zurich, Switzerland, Brandon Dugan, Rice University, Houston, TX, United States, Pierre Henry, CEREGE - Col France, Aix-En-Provence, France, Maria Jose Jurado, Instituto de Ciencias de la Tierra Jaume Almera, Barcelona, Spain, Kyuichi Kanagawa, Chiba University, Chiba, Japan, Toshiya Kanamatsu, JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan, Gregory F Moore, University of Hawaii at Manoa, Honolulu, HI, United States, Giuliana Panieri, University of Tromsø, Tromsø, Norway and Gian Andrea Pini, University of Trieste, Trieste, Italy
Mulitbeam swath bathymetry and reflection seismic data image large submarine landslide complexes along ocean margins worldwide. However, slope failure initiation, acceleration of motion and mass-transport dynamics of submarine landslides, which are all key to assess their tsunamigenic potential or impact on offshore infrastructure, cannot be conclusively deduced from geometric expression and acoustic characteristics of geophysical data sets alone, but cores and in situ data from the subsurface are needed to complement our understanding of submarine landslide dynamics. Here we present data and results from drilling, logging and coring thick mass-transport deposits (MTDs) in the Nankai Trough accretionary prism during Integrated Ocean Drilling Program (IODP) Expeditions 333 and 338. We integrate analysis on 3D seismic and Logging While Drilling (LWD) data sets, with data from laboratory analysis on core samples (geotechnical shear experiments, X-ray Computed Tomography (X-CT), Scanning Electron Microscopy (SEM) of deformation indicators, and magnetic fabric analysis) to study nature and mode of deformation and dynamics of mass transport in this active tectonic setting. In particular, we show that Fe-S filaments commonly observed on X-ray CT data of marine sediments, likely resulting from early diagenesis of worm burrows, are folded in large MTDs and display preferential orientation at their base. The observed lineation has low dip and is interpreted as the consequence of shear along the basal surface, revealing a new proxy for strain in soft sediments that can be applied to cores that reach through the entire depth of MTDs. Shear deformation in the lower part of thick MTDs is also revealed from AMS data, which – in combination with other paleo-magnetic data - is used to reconstruct strain and transport direction of the landslides.