Compared to the middle Okinawa Trough, magmatic features hold lower temperature and density and higher pressure and viscosity in the northern Okinawa Trough.

海槽北段岩浆的物理性质与南段相比具有温度低、压力高、密度小、粘度高的特征。

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Compared to the middle Okinawa Trough, magmatic features hold lower temperature and density and higher pressure and viscosity in the northern Okinawa Trough.

海槽北段岩浆的物理性质与南段相比具有温度低、压力高、密度小、粘度高的特征。

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