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The double-headed arrow beneath the KPR indicates an area of middle crust with Vp of 6.0 6.8 km/s.
The double-headed arrow indicates a region of middle crust with Vp of 6.0 to 6.8 km/s.
The double-headed arrow indicates a region of middle crust with Vp of approximately 6.3 to 6.8 km/s.
The double-headed arrow indicates a middle crust with Vp of approximately 6.3 to 6.8 km/s for each profile.
A middle crust with a V p of 6.1 6.6 km/s is estimated beneath the island arc and forearc area.
Crust thicker than 18 km also has over 5 km of middle crust with Vp of 6.0 to 6.8 km/s.
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Furthermore, a middle crust layer with a V P of 6.0 6.8 km/s is not unique to the IBM arc; it has also been documented in other intra-oceanic arcs such as the Tonga arc (Crawford et al., 2003) and the Kuriles (Nakanishi et al., 2009).
The velocity models show a complex crust, with a specially complex middle crust, which features higher velocities than the average continental crust.
The crustal thickness beneath the KPR is about 10 km with a middle crust of 2 km.
Fig. 1 Schematic strength profiles for the different types of crust in the South China Sea. a Strong crust offshore southern Hainan, b typical crust of southern China before rifting with thick weak middle crust, c crust under the Baiyun Sag at the time of low crustal flow.
On the other hand, a small bathymetric high exists to the west of Komahashi-Daini Seamount at a distance of 200 km, and it has a slightly thicker curst with no thick middle crust layer.
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