Sentence examples for outer ridges from inspiring English sources

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Multichannel seismic reflection data have shown that a mega-splay fault branching from the master décollement formed these outer ridges (e.g., Park et al. 2002; Moore et al. 2007).

The central Nankai Trough region, including the study area, is characterized by NE-SW-trending continuous outer ridges and elongated depressions separating the prism slope from the Kumano forearc basin (Figure 1).

The outer ridge is developed between splay fault and WBSF.

However, the degree of strain partitioning at the outer ridge has not been well quantified.

(c) 3D seafloor bathymetry showing outer ridge and WBSF (yellow arrowheads).

(a) Seafloor traces of the mega-splay fault at the outer ridge off Kumano.

This megasplay fault reaches the seafloor just seaward of the outer ridge.

The extracted fault geometry is discontinuous and en echelon with faults branching trenchward from beneath the outer ridge (Figure 4a,c).

Landward from this outer ridge off Kii Peninsula, the forearc Kumano Basin sediments unconformably cover the older accreted sediments (Figure 1b).

The high-resolution seafloor bathymetry indicates the presence of approximately 3.5- to 5-km-long linear depression landward of the outer ridge (yellow arrows in Figure 5).