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关注：1
2013-05-23 12:21
求翻译：Analogous mechanism was described in carbon saturation in C–O–H fluids during cold subduction of oceanic lithosphere [39]. Formation of diamonds occurred at low pressures and about 600 °C, when rock-buffered C–O–H crustal fluid reached the excess concentration of C required for the spontaneous nucleation of diamond.是什么意思？ 待解决
 悬赏分：1
- 离问题结束还有
Analogous mechanism was described in carbon saturation in C–O–H fluids during cold subduction of oceanic lithosphere [39]. Formation of diamonds occurred at low pressures and about 600 °C, when rock-buffered C–O–H crustal fluid reached the excess concentration of C required for the spontaneous nucleation of diamond.
问题补充： |
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2013-05-23 12:21:38
类似的机制在大洋岩石圈[39]冷俯冲在C-O -H流体饱和碳描述。
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2013-05-23 12:23:18
所述类似机制的碳饱和度在C-O-H液体潜没在寒冷的海洋岩石圈[39]。 钻石的形成发生在低压力和约600°C,当坚如磐石的缓冲C-O-H地壳流体达到超过浓度所需的C母液的自发的钻石。
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2013-05-23 12:24:58
近似机制在碳饱和在C-O-H流体被描述了在海洋陆界期间39的冷的算术的减法 ()。 当岩石缓冲的C-O-H地壳流体到达了为金刚石的自发生核，需要的C的剩余集中金刚石的形成发生了在低压和大约600 °C。
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2013-05-23 12:26:38
碳饱和 C — O — — H 流体中冷俯冲的大洋岩石圈 [39] 描述了类似的机制。钻石形成发生在低压力和大约 600 ° C，当岩石缓冲 C — O — — H 地壳流体可达 C 钻石自发成核所需的过剩浓度。
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2013-05-23 12:28:18
正在翻译，请等待...
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