期刊
GEOPHYSICAL RESEARCH LETTERS
卷 31, 期 12, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2004GL020136
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New swath bathymetry plus existing geophysical data reveal that the direction of West Philippine Basin (WPB) seafloor spreading rotated 100degrees counter-clockwise between 49 Ma and 33 Ma. The curvilinear and multi-stranded Mindanao Fracture Zone separates the WPB from the Palau Basin to the south. WPB opening was contemporaneous with, and behind, early Izu-Bonin-Mariana (IBM) subduction, whose arc volcanism began by 50 Ma. This produced over 1000 km of arc parallel spreading ( or stretching plus magmatism) in the Mariana segment of the Eocene IBM arc/forearc. The initial IBM subduction cut across, rather than followed, pre-existing structures (remnant arcs, fracture zones and spreading fabric). New models of subduction initiation are required to reproduce such characteristics.
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