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The crustal thickness beneath the KPR is about 10 km with a middle crust of 2 km.
The tonalite complex seems to correspond to this middle crust of the intra-oceanic island arcs with Vp of around 6 km/s.
The middle crust of the Oki-Daito Rise is thin compared to that at other bathymetric highs in this region (Figure 9a).
The most prominent feature imaged by the seismic survey is the Iberseis Reflective Body (IRB), a 140 km long high amplitude reflective body located in the middle crust of the northern half of the transect.
The top of the middle crust of the Amami Plateau (Figure 3) tends to shallow southward of the Kita-Daito Basin, particularly in the mid-row bathymetric high along DAr2.
In contrast, the neotectonically active ISTL could be associated with the underthrusting of the accreted parts by the middle crust of the Izu-Bonin arc in the middle Miocene to Pleistocene.
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Tamura et al. (2009) suggested that horizontal dykes in the crust could explain small spatial-scale variation of the middle crust on the basis of crustal structures, seismic reflectors, and petrological information.
The Vp model beneath the KPR for KPr11 shows a total crustal thickness of around 13 km, a middle crust thickness of about 5 km, Vp at the bottom of lower crust of 7.2 km/s, and Pn velocity of 7.6 km/s.
Crust thicker than 18 km also has over 5 km of middle crust with Vp of 6.0 to 6.8 km/s.
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.
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