岛弧形成于两个板块之间的活跃边界上，其中一块会被推挤到另一块的下方(称之为“消亡”)。
Island arcs form along an active boundary between two tectonic plates, with one being driven beneath the other (subduction).
岛弧形成于两个板块之间的活跃边界上，其中一块会被推挤到另一块的下方(称之为“消亡”)。
Island arcs form along an active boundary between two tectonic plates, with one being driven beneath the other (subduction).
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