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希望本篇文章《沿东太平洋上升段的轴向过程,10°–12°N》能对你有所帮助!
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本文概览: 东太平洋上升的轴向段由单个火山组成。每个火山都有独特的岩浆成分,并显示出沿着距中央腔轴的距离的分数结晶的系统变化。沿轴的热液排气,熔岩形态和构造也有所不同。熔岩从重叠扩散中...