Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean
Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean
复制标题
DOI:
10.1007/978-90-481-8885-7_1
复制
发表时间:
2011-01-01
期刊:
影响因子:
--
通讯作者:
Nakanishi, Masao
中科院分区:
文献类型:
--
作者:
Nakanishi, Masao
Elongated topographic structures associated with bending of the subducting oceanic plate along the western Kuril, Japan and northern Izu-Ogasawara trenches, were investigated using available multibeam bathymetric data. Magnetic anomaly lineations were also reidentified using available geomagnetic data to reveal controlling factors for strikes of bending-related topographic structures. The new bathymetric map demonstrates that most of bending-related topographic structures exist in the oceanward trench slopes deeper than 5,600 m. The map reveals that bending-related topographic structures are developed parallel to the trench axis or inherited seafloor spreading fabrics. Detailed identification of magnetic anomalies reveals curved lineations and discontinuity of lineations associated with propagation ridges. A trough with elongated escarpments associated with the propagating ridge in mid-Cretaceous Quiet Period was discovered near the trench-trench-trench triple junction. Comparison between the detailed bathymetric and magnetic anomaly lineation maps elucidates that abyssal hill fabrics were reactivated where the angle between abyssal hill fabrics and trench axis is less than about 30 degrees. The topographic expression of bending-related structures are classified into two types according to whether new faults develop parallel to the trench axis or inherited seafloor spreading fabrics reactivate.