在隐没带,当更老的和更冷的海洋地壳下降到另一个构造板块下面时,深震源地震可能会发生在非常深的深度(达到700公里)。
In subduction zones, where older and colder oceanic crust descends beneath another tectonic plate, Deep focus earthquakes may occur at much greater depths (up to seven hundred kilometers).
在隐没带,当更老的和更冷的海洋地壳下降到另一个构造板块下面时,深震源地震可能会发生在非常深的深度(达到700公里)。
In subduction zones, where older and colder oceanic crust descends beneath another tectonic plate, Deep focus earthquakes may occur at much greater depths (up to seven hundred kilometers).
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