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Jackson School of GeosciencesUTIG logo
Institute for Geophysics
Department of Geological SciencesBureau of Economic GeologyInstitute for Geophysics
A 3-D Seismic Investigation of the Nankai Trough Plate Boundary System in the Kumano Basin

Collaborative Research:
A 3-D Seismic Investigation
of the Nankai Trough Plate Boundary System
in the Kumano Basin


Principal Investigators:

Nathan Bangs

UTIG

Sean Gulick

UTIG

Greg Moore

University of Hawaii

Demian Saffer

Pennsylvania State Univ University Park

Harold Tobin

New Mexico Institute of Mining and Technology

Funding Agency: National Science Foundation

Abstract:
The PI team will acquire, process, and interpret a high-quality 3-D seismic reflection data volume in the Kumano Basin region south of Kii Peninsula, Japan. The 3D seismic survey will be carried out in April 2006 by PGS ship R/V Ramform Victory (Norwegian registry), jointly supported by the NSF and JAMSTEC. These data will define the fundamental geometry, history and physical properties of the multiple faults that compose the up-dip end of the seismogenic zone, many of which ruptured in the 1944 M 8.1 Tonankai earthquake. The proposed work is a major component of the integrated Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE), including the recently highly ranked shallow non-riser drilling and the deep riser drilling planned through the Integrated Ocean Drilling Program (IODP). With ground-truth from drilling and associated borehole geophysical experiments, this 3D seismic volume will provide unprecedented illumination of a plate boundary fault system to visualize its geometry, history, and associated rock properties, as it evolves down dip into a seismogenic zone. Furthermore, 3D imaging and seismic attribute mapping are essential components for refining drill site locations and for detailed planning for drilling and casing operations in support of the most ambitious scientific ocean drilling operation ever conceived. This project is a collaborative effort among four U.S. and two Japanese institutions to contract a seismic company to collect and provide preliminary processing of an ~20x80 km 3-D seismic reflection grid, along a transect from the Kumano Basin to the frontal thrust of the Nankai accretionary prism. The study encompasses a number of broader impacts, including the societal benefit of better understanding the origin of dangerous subduction zone thrust earthquakes.


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