Geochemistry of the Chaokeshan ophiolite: Product of intra - oceanic back - arc basin?

内蒙朝克山蛇绿岩地球化学: 洋内弧后盆地的产物?

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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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The isotopic dating and fossil geochronometry are the basic methods of ophiolite geochronometry.

同位素测年及化石年代学法是蛇绿岩年代学研究的基本方法.

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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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The small ocean basin is formed and the ophiolite appear when back arc basin expands.

弧后盆地扩张到达小洋盆,出现蛇绿混杂岩.

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