The volcano-graben basins are the most active fields for the tectonic-magmatic-geothermal system.
火山断陷盆地是构造-岩浆-地热体系的最活跃场所。
There is not the contemporary plate-tectonic system in the researching area. However, the active forms of polycycle trough (basin) developed in the area.
本区不存在现代板块构造体系，而具有多旋回海槽(盆)的活动形式。
There is not the contemporary plate-tectonic system in the researching area. However, the active forms of polycycle trough (basin) developed in the area.
本区不存在现代板块构造体系，而具有多旋回海槽(盆)的活动形式。
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