Tectonic landform and geological structure survey in the Toyama Trough.
Hydrograph1c Department of Japan conducted multichannel seismic reflection and refraction survey and Sea Beam bathymetric survey in the Toyama Trough extending northward in the southeastern margin of the Japan Sea. The purpose of the survey is to reveal the geological structure and tectonic landform of the Toyama Trough and to confirm the hypothesis that the Toyama Trough is a subduction zone. Another purpose of this study is to establish a refraction survey system using ocean bottom seismometers for revealing deep crustal structure, and to develop new method for image mapping of Sea Beam bathymetry which clearly shows topographical feature caused by tectonic deformation. Seismic profiles across the Toyama Trough do not support the presence of distinct subduction zone along the trough because the basement of the trough is not traceable beneath the Sado Ridge. This suggests that the Toyama Trough is different in geological feature from typical subduction zone such as the Japan Trench or the Nankai Trough, where subducting oceanic basement is clearly traceable beneath the overriding plate in seismic profiles. Further, seismic profiles show that the sedimentary layers thicken to the east in some places and to the west in the other places. These features indicate that convergent plate boundary is not present, or only extremely incipient plate boundary is present along eastern margin of the Toyama Trough However, the tectonic landform and geological structure characterized by the presence of active reverse faults indicate that Toyama Trough has been subjected to compressional stress.
| Main Authors: | , , |
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| Format: | Journal Contribution biblioteca |
| Language: | Japanese |
| Published: |
1989
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| Online Access: | http://hdl.handle.net/1834/16075 |
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