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Seitaro Ono

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Open access Oct 2026

Tectonic Evolution of the Mariana Trough

The Mariana Trough is an active back‐arc basin formed by subduction of the Pacific Plate beneath the Philippine Sea Plate and provides an ideal setting for investigating the evolution of back‐arc basins. In this study, we compile bathymetric, magnetic, and gravity data to reconstruct the formation history of the enti...

Seitaro Ono, Kyoko Okino, N. Seama et al. · Journal of Geophysical Resea... · 0 citations