The ophiolite partly formed ocean ridge, mainly formed in an ocean island.

蛇绿岩环境分析表明,部分为洋中脊环境, 大部分为洋岛环境.

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Generally speaking, we can not see the ocean ridge on the sea.

一般情况下, 我们在海面上是看不到海岭的.

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Seamounts, underwater volcanoes, Rift Valley, the mid - ocean ridge, constitute a rich world of the ocean floor.

海底山脉 、 海底火山 、 裂谷 、 大洋中脊等等, 构成了丰富的海底世界.

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Characteristics of trace and earth elements suggest that Ophiolite originated from the setting similar to - ocean ridge.

微量元素和稀土元素特征显示蛇绿岩形成于类似洋中脊的构造环境.

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A mid - ocean ridge a boundary between plates where new lithospheric material is injected from below s.

一道中海脊是板块之间的边界,在那里新的岩石圈的物质从下部注入.

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