Sagot :
6.5 cm/yr
The Nankai Trough is formed by subduction of the Philippine Sea plate (PSP) to the northwest beneath the Eurasian plate at a rate of 4.1–6.5 cm/yr (Figure 4.4.
6.5 cm/yr
The Nankai Trough is formed by subduction of the Philippine Sea plate (PSP) to the northwest beneath the Eurasian plate at a rate of 4.1–6.5 cm/yr (Figure 4.4.